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Annotated bibliography of Florida basement geology and related regional and tectonic studies

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Annotated bibliography of Florida basement geology and related regional and tectonic studies including an appendix of Florida deep well data ( FGS: Information circular 98 )
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FGS: Information circular
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Lloyd, Jacqueline M
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Tallahassee
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72 p. : ; 23 cm.

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Geology -- Bibliography -- Florida ( lcsh )
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Gulf of Mexico ( local )
Miami metropolitan area ( local )
City of Tallahassee ( local )
Pumpkin Bay ( local )
Atlantic Ocean ( local )
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Gulf of Mexico ( local )
South Florida ( local )
Basements ( jstor )
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Bibliography: p. 39-40.
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Includes indexes.
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by Jacqueline M. Lloyd.

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Full Text
STATE OF FLORIDA DEPARTMENT OF NATURAL RESOURCES
Elton J. Gissendanner, Executive Director
DIVISION OF RESOURCE MANAGEMENT Charles W. Hendry, Jr., Director
BUREAU OF GEOLOGY Steve R. Windham, Chief
INFORMATION CIRCULAR NO. 98
ANNOTATED BIBLIOGRAPHY OF FLORIDA BASEMENT
GEOLOGY AND RELATED REGIONAL AND TECTONIC STUDIES
INCLUDING AN APPENDIX OF FLORIDA DEEP WELL DATA
By
Jacqueline M. Lloyd
Published for the FLORIDA GEOLOGICAL SURVEY TALLAHASSEE
1985




ACE
DEPARTMENT
OF
NATURAL RESOURCES
BOB GRAHAM Governor
GEORGE FIRESTONE JIM SMITH
Secretary of State Attorney General
BILL GUNTER GERALD A. LEWIS
Treasurer Comptroller
RALPH D. TURLINGTON DOYLE CONNER Commissioner of Education Commissioner of Agriculture
ELTON J. GISSENDANNER
Executive Director








LETTER OF TRANSMITTAL


BUREAU OF GEOLOGY
TALLAHASSEE
April 15, 1985

Governor Bob Graham, Chairman
Florida Department of Natural Resources
Tallahassee, Florida 32301
Dear Governor Graham:
The Bureau of Geology, Division of Resource Management, Department
of Natural Resources, is publishing as its Information Circular No. 98,
"Annotated Bibliography of Florida Basement Geology and Related
Regional and Tectonic Studies."
This report summarizes published data on Florida basement geology and
includes an appendix of deep well data. As such, it is a comprehensive
reference publication for scientists studying Florida's deep geologic strata.
Respectfully yours,

Steve R. Windham, Chief
Bureau of Geology




Printed for the
Florida Department of Natural Resources
Division of Resource Management
Bureau of Geology
Tallahassee
1985




CONTENTS
Abstract...................................................................................................VI
Introduction........................ .................................................................... 1
Florida Basement Studies....................................................................... 2
Related Regional and Tectonic Studies............................................... 19
References...................... ........................................................................39
Author Index.......................................................................................... 41
Subject Index.........................................................................................43
Appendix-Florida Deep W ell Data.........................................................49




ABSTRACT
Annotated bibliographies of Florida basement geology and related regional and tectonic studies are presented along with an appendix containing Florida deep well data.
The bibliography of Florida basement geology is a comprehensive reference list. It includes published descriptions of some of the first deep wells drilled in Florida (e.g. Campbell, 1939 and 1940; Cole, 1944) as well as recent tectonic interpretations of the Florida basement. Other topics include the stratigraphy, geochronology, paleontology, and geophysical signature of Florida basement rocks.
The bibliography of related regional and tectonic studies includes papers on the Caribbean, Bahamas, Gulf of Mexico and West Africa. This section is not a complete reference list on these subjects. It is provided as a source for background information for the geologist working on the Florida basement.
Well cutting and core information is summarized in the appendix. These cutting and core samples are the basis for interpretation of Florida basement geology. References for published information on these samples are given; the samples themselves are available for further examination at the Florida Bureau of Geology.




ANNOTATED BIBLIOGRAPHY OF FLORIDA BASEMENT
GEOLOGY AND RELATED REGIONAL AND TECTONIC STUDIES
by
Jacqueline M. Lloyd
INTRODUCTION
This annotated bibliography is in two sections: one includes Florida basement studies, the other includes related regional and tectonic studies. Florida basement is generally thought of as including only pre-Mesozoic rocks. However, more specific, and potentially more useful, definitions are found in the cited literature. A consensus defines Florida basement as including igneous and metamorphic rocks of Precambrian and Paleozoic age, sedimentary rocks (primarily red beds) with associated intrusives and extrusives of Jurassic and Triassic (?) age, and unmetamorphosed sedimentary rocks of Paleozoic age. Although some of the authors may define basement differently,-each paper in the Florida basement section seems to fit somewhere within this definition. The papers in this section include studies of the petrography, lithology, stratigraphy, geochronology, and paleontology of Florida basement rocks. It also includes papers on the geophysical signature and geotectonic history of the Florida basement.
The second section of the bibliography includes papers covering the regional geology and tectonic history of the Caribbean, Bahamas, Gulf of Mexico, and West Africa. Some of these papers do not directly discuss the Florida basement. They are included because they provide information pertinent to Florida basement geology. Examples are Anderson and Schmidt (1983) and Dillon and Sougy (1974). Anderson and Schmidt (1983) present a model for the evolution of the Gulf of Mexico-Caribbean region. Florida's present and probable Paleozoic position tie it to such models. Dillon and Sougy's (1974) paper is a detailed reference on West African geology and geologic history from Paleozoic to present. It provides information that can be useful in reconstructing the Paleozoic position of Florida.
The appendix contains tabulated data on Florida deep wells which penetrated basement rocks. The data includes location, total depth, depth to basement, type of basement rocks, and references containing information on the particular basement rocks. Other pertinent data, such as age determinations, are listed if available. Well location maps are available from the Florida Geological Survey.




2 BUREAU OF GEOLOGY
FLORIDA BASEMENT STUDIES
ANDRESS, NOEL E., FRITZ H. CRAMER, and ROBERT F. GOLDSTEIN, 1969, Ordovician chitinozoans from Florida well samples: Gulf Coast Association of Geological Societies Transactions, vol. 19, pp. 369-375.
Ordovician chitinozoans recovered from a grayish black shale are described for the first time for subsurface north-central Florida. The bottom-most sample of Sun Oil Company, Earl Odom No. 1 well, Suwannee County, Florida, was bracketed as Late Arenigian to Early Caradocian. The Ordovician is immediately overlain by Silurian sediments. A new chitinozoan species is described. (authors' abstract)
APPLEGATE, ALBERT V., GEORGE O. WINSTON, AND JAMES G. PALACAS, 1981, Subdivision and regional stratigraphy of the Pre-Punta Gorda rocks (Lowermost Cretaceous-Jurassic?) in South Florida:
Supplement to Transactions-Gulf Coast Association of Geological Societies, vol. 31, pp. 447-453.
In recent years several wells have been drilled in the South Florida Basin through carbonate and evaporite sequences to depths as much as 5,300 feet below the Punta Gorda Anhydrite. Correlation of anhydrite beds below the Punta Gorda has revealed several thick anhydrite units (200 to 400 ft.) with regional persistence.
The pre-Punta Gorda section is subdivided into four easily identifiable units listed in order of increasing age-Lehigh Acres (lowermost Comanchean), Pumpkin Bay (upper Coahuilan), Bone Island (lower Coahuilan), and Wood River (Jurassic?) formations, all newly named in this report. In addition, the Lehigh Acres is divided into the West Felda Shale (base), Twelve Mile, and Able members which are also named and defined in this report. Geochemical evidence indicates that the Lehigh Acres unit and the upper part of the Pumpkin Bay unit contain the most likely source beds for petroleum.
Only two production tests have been carried out in the basin in strata below the oil-productive Sunniland Limestone. One was through casing in a Wood River dolomite zone. It reportedly produced water and some gas. The other was a drill stem test in an upper Pumpkin Bay dolomite zone which produced only water. In the Gulf Florida State Lease 826Y (Permit No. 275), a moderately porous, 350-feet-thick Pumpkin Bay dolomite zone was observed. As this well is west of the axis of the basin, better reservior conditions presumably exist on the West Florida shelf than onshore. (authors' abstract)
APPLIN, PAUL L., 1951, Preliminary report on buried pre-Mesozoic rocks in Florida and adjacent states: U.S. Geological Survey Circular No. 91, 28 p.
This paper is a basic reference work on the subsurface pre-Mesozoic rocks in Florida and adjacent portions of Alabama and Georgia. Available drill hole data is tabulated for 100 deep wells: 78 wells that penetrated




INFORMATION CIRCULAR NO. 98 3
Paleozoic sedimentary rocks, 18 wells that encountered Triassic (?) diabase and basalt (8 of these are included in the 78 that reach Paleozoic sedimentary rocks), and 12 significant deep wells that did not penetrate pre-Mesozoic rocks. These data are used to geographically divide the pre-Mesozoic subsurface into areas characterized by (1) Paleozoic sedimentary rocks, (2) extrusive igneous rocks (rhyolite, tuff, and agglomerate), and (3) intrusive igenous rocks (granite, diorite) and metamorphic rocks.
APPLIN, PAUL L., and ESTHER R. APPLIN, 1965, The Comanche Series and associated rocks in the subsurface in central and south Florida: U.S. Geological Survey Professional Paper 447, 86 p.
This paper is primarily a discussion of the Coastal Plain Mesozoic sedimentary section in Florida, however, some information on pre-Mesozoic rocks is included. The Coastal Plain floor in central and northern Florida is a truncated surface composed of igneous and sedimentary rocks. These rocks are tentatively classified as primarily early Paleozoic and Precambrian although some may be Triassic in age. The effect of the pre-Coastal Plain structure and topography on the major and minor structural features of the Comanche Series is discussed. ARDEN, DANIEL D., JR., 1974, Geology of the Suwannee Basin interpreted from geophysical profiles: Gulf Coast Association of Geological Societies Transactions, vol. 24, pp. 223-230.
Deep drilling in the eastern Gulf Coast has penetrated the Tertiary and Mesozoic section, but wells have seldom extended very deeply into pre-Mesozoic rocks. Data relating to the deeper pre-Mesozoic section were collected when Geophysical Service, Inc., conducted a seismic reflection survey in the Suwannee Basin (also called the Apalachicola Embayment or the Southwest Georgia Embayment). Associated gravity and magnetic field measurements were taken. The seismic sections provided the framework for initial geologic interpretation. Drilling data established stratigraphic control for the upper part of the sections and verified interval velocity determinations. A computer program generated gravity and magnetic fields for each hypothetical geologic interpretation. These were compared with the observed fields and refinements were made until data were reconciled.
The final interpretation shows Tertiary and Cretaceous sediments lying above a remarkably smooth unconformity developed upon Paleozoic and Triassic rocks. The unconformity dips southward from a depth of 8,400 feet near the Alabama-Florida boundary to about 12,000 feet near Panama City, Florida. Below the unconformity is a folded and faulted sequence of Lower Paleozic rocks and Triassic continental red beds accompanied by volcanic flows or intrusives. Paleozoic rock types include volcanics, quartzite, and a sandstone-shale sequence. Individual structures suggest broad anticlines developed above thrust faults. The Paleozoic rocks are tentatively correlated with (oil-producing) African counterparts, and it is suggested that their hydrocarbon potential warrants further investigation. (from authors' abstract)




4 BUREAU OF GEOLOGY
BANKS, J. E., 1978, Southern Florida-subsurface features related to oil exploration: Gulf Coast Association of Geological Societies Transactions, vol. 28, part 1, pp. 25-30.
Along one trend in southern Florida, 12 oil fields have been found, with an estimated 250 million stock-tank barrels of oil-in-place. Continued discovery of oil and gas in new fields and along new trends may be partly insured by structural mapping of the three types of basement rocks under peninsular Florida; by testing the first porosity in Paleozoic basement; by projecting the structural influence of basement troughs, paleovalleys, ridges and hills into overlying sediments; by distinguishing between two interfingering sedimentary platforms above basement-a northern one deposited on a convex floor, and a thicker, somewhat lower southern one overlying a flat-to-concave floor. (from authors' abstract)
BARNETT, RICHARD S., 1975, Basement structure of Florida and its tectonic implications: Gulf Coast Association of Geological Societies Transactions, vol. 25, pp. 122-142.
Geologic data from nearly 80 recent wells (1965 through 1975) in Florida and Georgia permit substantial refinement of earlier interpretations of Florida basement structure.
Upper Jurassic, Cretaceous, and Tertiary sediments in Florida onlap the eroded surface of a basement complex which varies from Precambrian to Jurassic in age. As determined by previous workers, the main structural feature underlying Florida is the Peninsular Arch. This is a large Precambrian block covered by Paleozoic sediments. A similar, smaller crustal block (the Decatur Arch or Chattahoochee Anticline), centering on Jackson County, occupies the Florida panhandle. In both blocks, Ordovician to Devonian clastic rocks overlie a deeply truncated Precambrian complex which was affected by Cambrian igneous intrusion. The Paleozoic rocks were subjected to Late Paleozoic uplift with some volcanic activity followed by uplift with tilting, block faulting and post-orogenic igneous intrusion during the Triassic period. The new data presented here clarify the succession and areal distribution of some of the volcanic and hypabyssal rocks, showing that Jurassic basalt flows covered the Peninsular Arch below the 280N parallel.
The entire Florida portion of the Florida-Bahama platform probably represents crust which has been continental throughout Phanerozoic time.
Subsurface data from Florida do not support the more speculative hypotheses about the history of the Florida-Bahama Platform and the Gulf of Mexico region. Published and new geologic data are consistent with responsible attempts to reconstruct the history of the Gulf of Mexico region by rifting during the opening of the North Atlantic Ocean basin. This agreement so far represents circumstantial evidence (general resemblance between early Paleozoic and Precambrian of Florida and west Africa) for the operation of plate tectonic mechanisms rather than direct, conclusive proof. The evidence, such as it is, favors the hypothesis outlined by Freeland and Dietz (1972). The circumstantial nature of evidence for the




INFORMATION CIRCULAR NO. 98 5
former activity of plate tectonic mechanisms in Florida need not hinder the application of new tectonic theories to petroleum exploration in Mesozoic rocks of the Florida-Bahama region and the outer continental shelf of the Atlantic coast. (authors' abstract; parenthetical comments added)
BASS, MANUEL N., 1969, Petrography and ages of crystalline rocks of Florida-some extrapolations: American Association of Petroleum Geologists Memoir No. 11, pp. 283-310.
The most widespread of the crystalline basement rocks of Florida are rhyolitic ignimbrites. Regional metamorphism has not affected the ignimbrites, and where greenschist-facies rocks are found the metamorphism is incomplete and local in extent. The age of the ignimbrites is unknown. Arguments are presented for Precambrian, late Paleozoic, Triassic, or Jurassic ages.
Intrusive rocks in Florida and Georgia are distributed sporadically except in an area of central Florida where a granitic province can be outlined. Granitic rocks are generally altered. In one well (Humble No. 1 Carroll, Sec. 10, T27S, R34E, Osceola County, P-8, W-1014), the quartz monzonite is cataclastically shattered and veined but not pervasively sheared. Another well (Sun No. 1, Powell Land Company, Sec. 11, T17S, R31E, Volusia County, P-19, W-1118) encountered a quartz-bearing hornblende diorite sill. This diorite is at least 480 m.y. old.
A province of mafic extrusive rocks is proposed for southern or southwestern Florida. The basalt resembles submarine basalt and may be related to buried seamounts. The basalt may be much younger than the acidic volcanic rocks.
The southeastern-most well (the Amerada No. 2, Cowles Magazines, Inc., Sec. 19, T36S, R40E, St. Lucie County, P-259, W-4323) penetrated diabase overlying, and in apparent fault contact with, regional metamorphic rocks. These rocks are mainly quartz-bearing hornblende-andesine amphibolite containing layers of leucocratic quartz diorite gneiss. This amphibolite is 530 m.y. old, or older. It is probably in a branch of the Damaran (or Pan-African) orogen. Meager data suggest that the diabase in this well may be of late Paleozoic, Triassic, or Jurassic age.
The age results for the various rock types indicate that an event about 530 million years ago resulted in amphibolite-facies and retrograde zeolite-facies metamorphism of mafic or intermediate igneous rocks in southern Florida. This event was probably accompanied by either metamorphism or emplacement of the quartz monzonite of the Carroll well and emplacement of the diorite of the Powell well. The country rocks intruded by the diorite were either Precambrian metamorphic rocks or sediments derived, at least partly, from Precambrian rocks.
BRIDGE, JOSIAH, and JEAN M. BERDAN, 1951, Preliminary correlation of the Paleozoic rocks from test wells in Florida and adjacent parts of Georgia and Alabama: U.S. Geological Survey Open File Report, 8 p., also in




6 BUREAU OF GEOLOGY
Florida Geological Survey Guidebook, Association American State Geologists 44th Annual Meeting Field Trip, April 1952, pp. 29-38.
Reported results are based on a preliminary study of cores, cuttings, and fossils from 52 test wells in central and northern Florida and adjacent parts of Georgia and Alabama. The subsurface Paleozoic rocks in this region include strata ranging from Early Ordovician to Early or possibly Middle Devonian. The area underlain by Paleozoic rocks can be roughly outlined by a triangle with sides approximately 250-miles long. It is bounded to the north and southeast by areas underlain by crystalline and volcanic rocks.
The Paleozoic strata are flat-lying, unmetamorphosed clastics, and were apparently deposited in shallow water. The source of the sediments is unknown. The total thickness of Paleozoic sediments is estimated to be not less than 3,000 feet and probably equal to 6,000 feet or more.
The distribution of Paleozoic rocks of different ages indicates the possibility that the wedge of Paleozoic rocks is made up of a series of subparallel belts, each with a general northeast trend, and each separated from adjacent belts by faults. The age of faulting is post-Middle(?) Devonian to pre-Early Cretaceous. Igneous intrusions cutting the Paleozoic sedimentary rocks fall within the same age limits.
CAMPBELL, R. B., 1939, Paleozoic under Florida?: American Association of Petroleum Geologists Bulletin 23, No. 11, pp. 1712-1713.
A brief report on the black shales found in the St. Mary's River Corporation Hilliard Turpentine Co. No. 1 well in Nassau County, Florida, is presented in this paper. The black shales are tentatively assigned a Mississippian age because of their similarity to the Chattanooga shales.
CAMPBELL, R. B. 1940, Outline of the geological history of peninsular Florida: Florida Academy of Science Proceedings, 1939, vol.4, pp. 87-105.
Previously unpublished data on eight Florida wells is presented. Paleogeographic changes (Cretaceous through Recent) of the Florida peninsula are depicted. The influence of the three "ancient nuclear land masses"-Appalachia, Llanoria, and Antillia-and the coverage by sea waters are discussed. The conclusion is that the "Florida peninsular area throughout most of its geologic history has been submerged and as such, has been the connecting link from the Gulf of Mexico to the Atlantic, between the nuclear land masses of Appalachia and Antillia, roughly represented today by the Piedmont area of the southern states and the Greater Antilles respectively."
CARROLL, DOROTHY, 1963, Petrography of some sandstones and shales of Paleozoic age from borings in Florida: U.S. Geological Survey Professional Paper 454-A, 15 p.
Sandstone, orthoquartzites, other arenaceous sediments and black and red shales occur in the basement rocks of Florida and adjacent parts of




INFORMATION CIRCULAR NO. 98 7
Georgia and Alabama. Most of the sandstones are Early Ordovician in age. The shales range in age from Middle Ordovician to Middle Devonian.
The quartzites range in mineralogic complexity from submature to mature. Feldspars are scarce. Micaceous and clayey sandstones can be classed as subgraywackes. Many of the quartzites grade into siltstones that are intercalated with shaly and micaceous layers. Such beds show disturbed bedding and penetration by worm borings. These beds may be of shallow-water marine origin.
All the arenaceous sediments contain small amounts of heavy minerals. Three characteristic heavy-mineral assemblages were recognized that could be used to correlate different beds in the sequence. The minerals indicate sources in granitic and metamorphic rocks, although rounding of the grains suggests that most of the rocks were derived finally from second- or third-cycle sediments.
The black shales contain abundant organic matter, pyrite, and commonly, interlaminations of siderite and calcite. The color of the red shales is due to minute blebs of hematite in the micaceous matrix. (from author's abstract and summary)
CHOWNS, T. M., and C. T. WILLIAMS, 1983, Pre-Cetaceous rocks beneath the Georgia Coastal Plain-regional implications: in Gohn, Gregory S. (editor), Studies related to the Charleston, South Carolina, earthquake of 1886-tectonics and seismicity: U.S. Geological Survey Professional Paper 1313-L, 42 p.
The records of 78 wells that have penetrated pre-Upper Jurassic(?) rocks beneath the Georgia Coastal Plan were analyzed and used as the basis for a regional interpretation of the "basement" of the southeastern U.S. Coastal Plain. These results were compared with the results of similar studies in Florida, Alabama, and South Carolina. With the addition of regional aeromagnetic data, regional interpretations were made.
Felsic volcanic and associated rocks found in the Georgia subsurface are identical to those found beneath the Apalachicola embayment in Alabama and the Florida panhandle, on the southeast flank of the Peninsular Arch in central Florida, and in south Florida. Evidence suggests that, aside from those found in south Florida, the volcanic rocks are Proterozoic Z (Late Proterozoic) or early Paleozoic in age. Available data indicate a Mesozoic age for the south Florida rocks. The Proterozoic to Paleozoic volcanic rocks probably represent a disjunct fragment of the African craton, sutured to North America during the late Paleozoic. The position of the suture is unknown, but the boundary between the Piedmont rocks of the Appalachian orogen and African platform rocks may be traced in the subsurface east-northeast from Alabama to South Carolina. Before the opening of the Atlantic, this boundary was continuous with the overthrust on the east side of the African Mauritanide orogenic belt.
The most extensive terrane beneath the Southeastern Coastal Plain is a broad basin (the South Georia Basin) filled with red beds, associated diabase intrusions, and possibly basalt. These red beds occupy an




8 BUREAU OF GEOLOGY
estimated 50,000-65,000 sq. km in Georgia and a similar area in adjacent parts of Florida, Alabama, and South Carolina. The diabase and basalt are Early Jurassic in age; the red beds are Late Triassic(?) to Early Jurassic(?). For simplicity, the red beds are referred to as Triassic. Much of this Triassic terrane has undergone zeolite-facies alteration. The alteration is most pronounced, but not restricted to, contact aureoles of the diabase bodies.
The Triassic terrane probably represents a complex graben structure, formed during the early stages of the opening of the North Atlantic (215-175 million years ago). The southeastern corner of North America was close to the triple junction between the North Atlantic, South Atlantic and the Gulf of Mexico, therefore, complex rifting and transform faulting would be expected. The position and size of the South Georgia basin, as well as the large volume of mafic igneous rock and evidence of high heat flow, suggest that during the Late Triassic and Early Jurassic, incipient spreading centers in the Gulf of Mexico and the North Atlantic may have been linked beneath this basin.
The Brunswick magnetic anomaly, which swings through South Georgia, is probably of late Paleozoic origin. It may be caused by a thick section of African-plate rocks, which was formed by overthrusting during continental collision. This similarity in trend between the early Mesozoic East Coast anomaly at the margin of the Carolina shelf and the Brunswick anomaly suggests that the position of the Atlantic spreading center may have been influenced by this Paleozoic structure. (partially extracted from authors' abstract)
COLE, W. STORRS, 1944, Stratigraphic and paleontologic studies of well~ in Florida-No. 3: Florida Geological Survey Bulletin No. 26,168 p.
This document includes a detailed stratigraphic and paleontologic description of the St. Mary's Oil Corporation, Hilliard Turpentine Company No. 1 well, Sec. 19, T4N, R24E, Nassau County (W-336, no permit number). The well was completed in 1940 at a depth of 4,817 feet. The well encountered a black shale at 4,640 to 4,795 feet and a diabase sill or dike at 4,795 to 4,817 feet. The black shale and the diabase are both believed to be Triassic in age, although the age of the shale has been the subject of much debate.
CRAMER, FRITZ H., 1971, Position of the North Florida Lower Paleozoic block in Silurian time; phytoplankton evidence: Journal of Geophysical Research, vol. 76, no. 20, pp. 4754-4757.
The Silurian reconstruction of Pangea leaves a space inside the divergence of the 1,000-fathom contours of the African and South American continental blocks. Palynological evidence suggest this space as a pre-Late Devonian location for the North Florida Lower Paleozoic block. It was brought to its present position with respect to the Appalachians when the proto-Atlantic closed in the Late Devonian.
CRAMER, FRITZ H., 1973, Middle and Upper Silurian chitinozoan




INFORMATION CIRCULAR NO. 98 9
succesion in Florida subsurface: Journal of Paleontology, vol. 47, no. 2, pp. 279-288.
Unmetamorphosed Paleozoic rocks are present in the subsurface of Florida. Silurian acritarchs, chitinozoans and miospores have been recovered from black to gray shales of four wells in the north-central portion of the state. On account of its palynomorphs, mainly chitinozoans, this material is dated as very latest upper Llandoverian though upper Ludlovian or very basal Gedinnian. The Florida ranges of 28 stratigraphically valuable chitinozoan taxa are plotted; nearly all taxa are illustrated by photomicrographs.
The Florida palynomorph spectra and their chronological succession are quite similar to age-equivalent material from Portuguese Guinea and, in part, to material from North Africa.
The palynological data suggest that the environment of deposition in north-central Florida was holomarine, and not lagoonal as was supposed before. (author's abstract)
GOLDSTEIN, ROBERT F., FRITZ H. CRAMER, and NOEL E. ANDRESS, 1969, Silurian chitinozoans from Florida well samples: Gulf Coast Association of Geological Societies Transactions, vol. 19, pp. 377-384.
Chitinozoans of Silurian age were recovered from four wells in north peninsular Florida: Humble-Cone No. 1 (Sec. 22, TIN, R17E, P-77, W-1789); Sun Oil-Tillis No. 1 (Sec. 28, T2S, R15E, P-57, W-1548); St. Mary's River-Hilliard No. 1 (Sec. 19, T4N, R24E, no permit number, W-336); and Gulf-Kie Vining No. 1 (Sec. 2, T4S, R15E, P-124, W-2164). An attempt was made to establish a correlation between these four wells using the chitinozoan evidence. The youngest assemblage encountered is probably Ludlovian in age; the oldest is of late Llandoverian age. (from authors' abstract)
GRASTY, R. L., and J. TUZO WILSON, 1967, Ages of Florida volcanics and of opening of the Atlantic Ocean: Tectonophysics Abstracts, American Geophysical Union Transactions, vol. 48, pp. 212-213.
Four basalts from Florida deep wells were obtained and dated. Ages ranged from 140 to 180 million years; the older age is believed to be more correct. It agrees with similar ages reported for basic intrusives along the coast. It is also compatible with the view that the North Atlantic Ocean began opening at that time and that the Florida-Bahamas ridge may have formed along the boundary with the pre-existing Gulf of Mexico. (from authors' abstract)
GRIFFIN, GEORGE M., DAVID A. REEL, and RICHARD W. PRATT, 1977, Heat flow in Florida oil test holes and indications of oceanic crust beneath the southern Florida-Bahamas platform: in Smith, Douglas L., and George M. Griffin (editors), The geothermal nature of the Florida Plateau: Florida Bureau of Geology Special Publication 21, pp. 43-64.
Heat flow values were obtained for three deep oil-test holes. Two test




10 BUREAU OF GEOLOGY
holes in southern Florida yielded values of 0.71 and 0.76 HFU*, one in northern Florida yielded a value of 0.92 HFU. This trend on land parallels a similar trend offshore and is approximately the same in magnitude. The low values for southern Florida support the hypothesis that oceanic crust (low heat generating capacity) underlies the southern part of the Florida-Bahamas platform.
"Note: 1 HFU (or heat flow unit) = 1 x 10-6 cal/cm2 sec. The average heat flow from continental areas is about 1.5 HFU.
KING, ELIZABETH R., 1959, Regional magnetic map of Florida: American Association of Petroleum Geologists Bulletin, vol. 43, pp. 2844-2854.
A regional magnetic map of Florida reflects the structural trends of the magnetically heterogeneous Paleozoic and Precambrian rocks underlying the coastal plain rocks. Many trends and features on the magnetic map have gravity counterparts, indicating a common source. On the basis of the regional magnetic trends, Florida is divided into two tectonic provinces with an intervening zone of intrusive rocks. Depth estimates from aeromagnetic data suggest the possibility that faulting may be a factor in the profound downwarping and accumulation of sediments in the southern province. The trends of the northern province parallel those of the Appalachian system to which they are probably related. The southern province, distinguished by northwest trends, is structurally discordant with the northern province. The magnetic evidence suggest that the southern province is a continuation of the Ouachita system which has been traced beneath the Gulf Coastal Plain to within 60 miles of the subsurface extension of the Appalachian system in Mississippi, where the two systems approach each other at nearly a right angle. (author's abstract)
KLITGORD, KIM D., PETER POPENOE, and HANS SCHOUTEN, 1984, Florida: a Jurassic transform plate boundary: Journal of Geophysical Research, vol. 89, no. B9, pp. 7753-7772.
Magnetic, gravity, seismic, and deep drill-hole data integrated with plate tectonic reconstructions substantiate the existence of a transform plate boundary across southern Florida during the Jurassic. On the basis of this integrated suite of data the pre-Cretaceous Florida-Bahamas region can be divided into the pre-Jurassic North American plate, Jurassic marginal rift basins, and a broad Jurassic transform zone including stranded blocks of pre-Mesozoic continental crust. Major tectonic units include the Suwannee basin in northern Florida containing Paleozoic sedimentary rocks, a central Florida basement complex of Paleozoic age crystalline rock, the west Florida platform composed of stranded blocks of continental crust, the south Georgia rift containing Triassic sedimentary rocks which overlie block-faulted Suwannee basin sedimentary rocks, the Late Triassic-Jurassic age Apalachicola rift basin, and the Jurassic age south Florida, Bahamas, and Blake Plateau marginal rift basins. The major tectonic units are bounded by basement hinge zones and fracture zones
(FZ). The basement hinge zone represents the block-faulted edge of the




INFORMATION CIRCULAR NO. 98 11
North American plate, separating Paleozoic and older crustal rocks from Jurassic rifted crust beneath the marginal basins. Fracture zones separate Mesozoic marginal sedimentary basins and include the Blake Spur FZ, Jacksonville FZ, Bahamas FZ, and Cuba FZ, bounding the Blake Plateau, Bahamas, South Florida and southeastern Gulf of Mexico Basins. The Bahamas FZ is the most important of all these features because its northwest extension coincides with the Gulf basin marginal fault zone, forming the southern edge of the North American plate during the Jurassic. The limited space between the North American and the South American/ African plates requires that the Jurassic transform zone, connecting between the Central Atlantic and the Gulf of Mexico spreading systems, was located between the Bahamas and Cuba FZ's in the region of southern Florida. Our plate reconstructions combined with chronostratigraphic and lithostratigraphic information for the Gulf of Mexico, southern Florida, and the Bahamas indicate that the Gulf was sealed off from the Atlantic waters until Callovian time by an elevated Florida-Bahamas region. Restricted influx of waters started in Callovian as a plate reorganization, and increased plate separation between North America and South America/Africa produced waterways in the Gulf of Mexico from the Pacific and possibly from the Atlantic. (authors' abstract)
KRIVOY, HAROLD L., and THOMAS B. PYLE, 1972, Anomalous crust beneath West Florida Shelf: American Association of Petroleum Geologists Bulletin, vol. 56, no. 1, pp. 107-113.
A new Bouguer gravity anomaly map of the west Florida continental margin reveals a landward salient of high positive values in the vicinity of St. Petersburg. A 20,000 sq km area of the shelf characterized by anomalies greater than +30 mgal is thought to be underlain by a crust having a thickness intermediate between that of continents and that of oceans. A transition from oceanic toward continental crust in this area may have been accomplished by reef progradation across an ancient oceanic embayment. Alternatively, a transition from continental toward oceanic crust may have been produced by rotation of Florida and consequent rifting. The reef-progradation hypothesis is most consistent with what is known of the deep structure and tectonic setting of the Florida platform. (authors' abstract)
MILTON, CHARLES, 1972, Igneous and metamorphic basement rocks of Florida: Florida Bureau of Geology Bulletin 55, 125 p.
This report describes in detail all the cores and cuttings available from a large collection of wells which were drilled in the Florida Coastal Plain, which penetrated rocks older than the Late Cretaceous, Tuscaloosa Formation. The petrography of basement rock from 27 Florida wells is described; also some 14 isotopic datings from six wells in Florida and three in Georgia, and chemical analyses of rocks from seven Florida wells are given.
Although many wells have been drilled into the Florida pre-Cretaceous




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14 BUREAU OF GEOLOGY
spathic sandstone and shale. A similar sequence of rocks is observed in Guinea, 200 km northeast of the west African shoreline; there the rocks, also sandstones and shales, are of the same age, Ordoviclan-Devonian. Similarly, they unconformably overlie a deformed and metamorphosed basement of pre-Cambrian and Cambrian age. These similarities between the Florida and Guinea terranes ... suggest their correlation and consequently, their relevance to pre-Atlantic reconstructions.
In the reconstruction of LePichon and others (1977) the two terranes are separated by several hundred kilometers. A more northerly position of Africa-South America with respect to North America results in a closer correspondence of the two terranes. Since the reconstruction of LePichon and others (1977) and the subsequent seafloor spreading history are well justified from marine data, the more northerly position of Africa was probably achieved in the latest Paleozoic or early Mesozoic, prior to opening of the present-day Atlantic Ocean. (author's abstract)
POJETA, JOHN, JR., JIRI KRIZ, and JEAN M. BERDAN, 1976, Silurian-Devonian pelcypods and Paleozoic stratigraphy of subsurface rocks in Florida and Georgia and related Silurian pelecypods from Bolivia and Turkey: U.S. Geological Survey Professional Paper 879, 32 p.
The subsurface sedimentary Paleozoic rocks beneath northern Florida and adjacent parts of Georgia and Alabama comprise a sequence of quartzitic sandstones and micaceous shales, dark-gray shales, and red and gray siltstones ranging in age from Early Ordovician to Middle Devonian. The Silurian-Devonian pelecypod faunas from four wells (three of which, the Ragland, Cone, and Tillis wells, are in Florida, and one of which, the Chandler, is in Georgia) are described and illustrated. Also described are Silurian pelecypods from one locality in Bolivia and one in Turkey.
Biostratigraphically, the faunas from the American wells range in age from Weniockian or Ludiovian (Silurian) to Middle Devonian; the Bolivian specimens are probably Ludlovian (Late Silurian); and the Turkish specimens are probably Wenlocklan or Ludlovian (Silurian). Paleocologically, the strata in the American wells represent shallow-water normal marine environments, and all pelecypods known from them belong to one of three life-habit groups-byssally attached, burrowing, or reclining. The Bolivian and Turkish pelecypods likewise belong only to these three life-habit groups. Analysis of the geographic distribution of the Florida Paleozoic pelecyod genera shows that they are closest to the forms found in central Bohemia and Poland; elements of this fauna also occur in Nova Scotia, North Africa, and South America. (authors' abstract)
SHERIDAN, ROBERT E., J. T. CROSBY, G. M. BRYAN, and P. L. STOFFA, 1981, Stratigraphy and structure of Blake Plateau, northern Florida Straits, and northern Bahama Platform from multichannel seismic reflection data: American Association of Petroleum Geologists Bulletin, vol. 65, pp. 2571-2593.




INFORMATION CIRCULAR NO. 98 15
Approximately 2,100 km of 24-fold multichannel seismic reflection data reveal much about the subsurface geology for a large part of the continental margin east of Florida. Discordance between the westward-dipping pre-breakup sediments and the eastward-sloping basement along the edge of the Blake Plateau is Interpreted as an effect of a splinter of continental margin derived from the African plate by a spreading-center jump in the Middle Jurassic. Early rafting centered under the main part of the Blake Plateau became Inactive, as a spreading-center jump shifted the active rift to east of the present Blake Escarpment along the Blake Spur magnetic anomaly.
In the northern Florida Straits -the data reveal that the breakup unconformity, underlain by Triassic-Lower Jurassic(?) arkosic volcaniclastics, extends from southern Florida to the western Bahama Banks. These volcaniclastics are associated with the rift-crust of Intermediate nature formed just prior to and during breakup of the North American and African continental plates.
Back-reef platform deposits of limestones, dolomites, and evaporites of Late Jurassic to Alblan age extend from the Blake-Bahamas Escarpment westward beneath Florida. These deposits formed what once was a megabank extending over a wider area than the present smaller isolated Bahamas Banks. The formation of the Florida Straits and Bahamas channels occurred during the Cenomanian transgression. Only on the present Bahamas Banks and Florida platform did shallow-water carbonate deposition persist to maintain a shallow-bank environment.
Evidence of recurring scour by current erosion is found in the Florida Straits. Erosional events apparently occurred in the middle Cenomanian, middle Paleocene, early-middle Eocene, and Eocene-Oligocene, which coincidentally are times of lower eustatic sea level according to Vail et al. (1977). This evidence of Florida current scour indicates that the currentwas present as far back as the Cenomanian.
Major faulting appears to have dropped the Northeast Providence Channel relative to the western Bahamas after the Alblan. Submarine erosion and bank buildup created the channels and smaller relief features like Great Abaco Knoll beginning in about the Cenomanian.
A carbonate bank margin and reef complex was present along the Bahamas Escarpment since the Middle Jurassic. Apparently these organic buildups seeded on originally shallow structural relief on oceanic basement created during the spreading-center jump to the position of the Blake Spur magnetic anomaly. The bank margin apparently has retreated at least 15 km from a Late Jurassic-earliest Cretaceous position now marked by a bench below the Au unconformity*.
Active faulting occurred along the Great Abaco fracture zone at.least through the Late Cretaceous and perhaps into the Tertiary. These relatively young tectonic events, together with the post-Albian faults in Providence
*Note: The Au reflector, or horizon, is a hiatus between lower Miocene and possibly Cenomanlan rocks.




16 BUREAU OF GEOLOGY
Channel, indicate interactions between the Atlantic and Caribbean plates and that extensions of faulting have taken place far to the northeast of Cuba and the Greater Antilles. (authors' abstract)
SHERIDAN, ROBERT E., C. L. DRAKE, J. E. NAFE, AND J. HENNION, 1966, Seismic refraction study of continental margin of Florida: American Association of Petroleum Geologists Bulletin, vol. 50, pp. 1972-1991.
Data from 31 seismic-refraction profiles are interpreted and presented in five structure sections. The subsurface structure east of Florida under the Blake Plateau is similar to that of the margin north of Cape Hatteras. Basement plunges seaward from Florida into a deep sedimentary trough under the Blake Plateau. A basement ridge parallels this north-southtrending trough on the seaward side, along the eastern edge of the plateau.
The basin under the Blake Plateau was separated from the South Florida-Andros Island basin,, at least until the Early Cretaceous, by a southeastward extension of the Peninsular Arch. This seaward extension trends from just east of Cape Kennedy to the western end of Little Bahamas Bank.
The marked relief of the Florida shelf, the Florida Straits, and the Blake Plateau is evident only in the sedimentary layers and is the result of significant changes in thickness of the post-Paleocene section, especially the Eocene. The top of the Paleocene extends beneath the present physiographic irregularities with slight relief, whereas the Eocene thickness ranges from about 500 m on Florida to about 70 m on the Blake Plateau. Strong currents sweeping the Florida Straits and Blake Plateau probably are responsible for the absence of a thick post-Paleocene section. The present orientation of the Florida current may have existed as early as Paleocene time.
Besides the changes in relief within the sedimentary section, there are lateral facies changes and velocity variations. These variations are primarily dependent on the depth of burial. Nearly similar velocity-depth distributions are found for the Blake Plateau, the Florida Straits, the Bahamas Banks, and the Florida Platform. The variations in thickness of the sediments in these areas result in variable velocities in the stratigraphic units, and correlation of the refraction data is difficult. (authors' abstract)
SMITH, DOUGLAS M., 1983, Basement model for the panhandle of Florida: Gulf Coast Association of Geological Societies Transactions, vol. 33, pp. 203-208.
Core samples from deep boreholes in panhandle Florida form the basis of a basement model involving at least eight separate fault blocks and basins, each with a distinct depositional history. The dominant structures are a northwest-trending fault and a large northeast-trending Triassic graben which encompasses several secondary fault blocks and forms the Southwest Georgia Embayment (Apalachicola Embayment). This graben as well as associated and perpendicularly-oriented (northwest-southeast) faults were formed in response to tensional forces related to the Mesozoic




INFORMATION CIRCULAR NO. 98 17
separation of North American and South American land-masses and the consequent formation of the Gulf of Mexico. Granitic basement blocks, perhaps Early Cambrian in age, experienced differential subsidence and changing relationships with various sedimentary source terrains. Thus, the separate basins accomodated different combinations of Triassic Eagle Mills red beds and Jurassic deposits ranging from the Louann Salt to the Cotton Valley sandstones and shales. (author's abstract)
SMITH, DOUGLAS M., 1982, Review of the tectonic history of the Florida basement Tectonophysics, vol. 88, pp. 1-22.
This paper provides a comprehensive review of the lithological, geochronological, paleontological, and geophysical data used to interpret the tectonic history of Florida. Comparison with similar data on African rocks yields a model for the tectonic history of the Florida basement. The author's abstract summarizes the model as follows:
"Lithological similarities between the Suwannee Basin deposits of undeformed Ordovician and Silurian sandstone and shale lying 0.9-1.9 km below the north Florida surface and equivalent-aged strata from Senegal to Sierra Leone in western Africa suggest an African location for the Florida basement during the early Paleozoic. The southern edge of the Paleozoic sediments laps onto a Pan-African granitoid batholith which is considered representative of a nearly Paleozoic Afro-South American assemblage. A late Paleozoic (Allegheny) continental closure brought the Florida basement, and much of the present-day Gulf Coastal margin, into juxtaposition with North America, but the arrangement of continental promontories precluded a direct application of deforming stresses to the overlying basin sediments. Numerous occurrences of early Mesozoic rhyolitic tuffs and ignimbrites in deep (2.7-5.5 km) bore holes from central and south Florida are interpreted as indicative of a Triassic hot spot that initiated rifting and the opening of the North Atlantic.
Subsurface rhyolitic rocks are also present in northern Florida, but the position of the hot spot dictated that the Florida Plateau remain appended to North America as radially propagating rifts from the hot spot created a new configuration of plate boundaries from those of the Paleozoic. Other continental terrains adjacent to southern Florida were either altered and foundered to underlie the
Bahamas or stayed with Africa and/or South America."
WALPER, JACK L., 1974, The origin of the Bahamas Platform: Gulf Coast Association of Geological Societies Transactions, vol. 24, pp. 25-30.
The origin of the Bahama platform and its continued subsidence to permit the accumulation of a thick carbonate cap has been a problem of middle American geology. The relation of this feature to previously published reconstructions of the late Paleozoic-early Mesozoic "fit" of North America, Africa and South America has also posed a problem. A new




18 BUREAU OF GEOLOGY
model incorporating the volcano-tectonic rift and ignimbrite sheet association is proposed to explain the origin of the Bahama platform as an integral part of Caribbean plate tectonics. A new North America-South America join is utilized to account for the major geologic and tectonic continuities of Paleozoic age throughout Mexico and Central America.
The clockwise rotation of North America as it separated from South America and Africa caused the counterclockwise bending of the entire peninsula of Mexico and Central America, with the newly accreted Caribbean plate into a subduction zone that was to evolve into the arc-trench system of the Greater Antilles. The rotation and beginning of subduction of this Caribbean plate into the Cuban trench, in Jurassic time, triggered volcanic eruptions that provided the foundations for the Cuban volcanic arc and the usual thick and widespread ignimbrite sheet behind the arc in the area now occupied by peninsula Florida and the Bahama Banks.
Not only is evidence for this feature found in wells drilled in Florida but it also provides the foundation upon which was deposited the thick sequence of carbonate strata that forms the Bahama Banks. This interpretation eliminates the overlap of the Bahama salient onto Africa, explains the origin of the Old Bahama Channel, serves the same purpose as the sedimentary prism proposed by Dietz and other (1970) and has the volcanic character to meet the geophysical requirements indicated by Uchupi and others (1971). (author's abstract)
WICKER, RUSSELL A., and DOUGLAS L. SMITH, 1977, Florida basement-an isometric view: American Association of Petroleum Geologists Bulletin, vol. 61, pp. 2143-2145.
An isometric view of the Florida basement surface, based on available core data from more than 150 boreholes, has been derived by application of the SYMAP and SYMVU computer programs. This visualization shows numerous topographic features which can be associated with structural patterns in the overlying formations and illustrates a significant contrast in basement depth between northern and southern Florida. (authors' abstract)
WICKER, RUSSELL A., and DOUGLAS L. SMITH, 1978, Reevaluating the Florida basement, Gulf Coast Association of Geological Societies Transactions, vol. 28, pp. 681-687.
A generalized representation of the basement and overlying sedimentary rocks of peninsular Florida has been developed utilizing available gravity anomaly values, deep test-well data, and a variation of the Talwani, et al. (1959) two-dimensional gravity modeling technique. Subsurface density and depth values along 10 profiles were adapted to an iterative calculating process to generate gravity anomaly profiles conforming to those observed. Modeled cross-sections along these profiles were then used to interpolate basement and sedimentary configurations for the entire peninsula. The final models display the low density (1.95-2.15 gm/cm3) near-surface rocks of Late Cretaceous to Recent ages extending to depths




INFORMATION CIRCULAR NO. 98 19
ranging from approximately 0.8 to 2.6 km. Depths of the underlying Lower Cretaceous rocks (density of 2.30 to 2.55 gm/cm3) extend to approximately 1.4 km in north Florida and more than 4.7 km in south Florida. An abrupt north-to-south increase in average basement rock density from 2.73 to 3.00 gm/cms is evident along a general east-west trending zone passing through the central portion of the peninsula. This supports a concept of a north-to-south transition from continental to oceanic type rocks underlying the thick sedimentary sequence of the central Florida peninsula. (authors' abstract)
WILSON, GARY V., 1975, Early differential subsidence and configuration of the northern Gulf Coast Basin in southwest Alabama and northwest Florida: Gulf Coast Association of Geological Societies Transactions, vol. 25, pp. 196-206.
Deep test-well information in southwest Alabama and northwest Florida indicates that early differential subsidence of the basement had a marked influence on the thickness and distribution of accumulating coastal plain sedimentary deposits, especially carbonates, evaporites and thick marine shale units. Geophysical data reveal that these differential movements were either directly or indirectly related to lateral variations in the thickness of crustal layers. These crustal thickness variations may have been either the cause of differential subsidence of the basement or the result of deep-seated forces that induced or affected subsidence. Regional gravity anomalies reflect crustal thickness variations associated with the Wiggins uplift and the Mississippi interior salt basin. In the study area a basement high and stratal thinning correspond to the easternmost extension of the Wiggins uplift and a regional gravity minimum. A basement low and stratal thickening correspond to the eastern limb of the Mississippi interior salt basin and a regional gravity maximum.
The configuration of the basin margin during much of Late Jurassic time was controlled by a hinge line that roughly coincided with a system of dense intracrustal masses. These masses probably locate a zone of structural weakness within the crust, basinward from which initial subsidence and marine deposition took place. The basin margin and extent of early marine deposition was also influenced by the Wiggins uplift and the related Conecuh arch. This influence continued until Cretaceous seas advanced beyond the northern extent of this positive feature. (authors' abstract)
RELATED REGIONAL AND TECTONIC STUDIES
ANDERSON, THOMAS H., and VICTOR A. SCHMIDT, 1983, The evolution of Middle America and the Gulf of Mexico-Caribbean Sea during Mesozoic time: Geological Society of America Bulletin, vol. 94, pp. 941-966.
A plate-tectonic model for the evolution of Middle America and the Gulf of Mexico-Caribbean Sea region is presented. The model, which is based upon the existence of the Mojave-Sonora megashear, incorporates into the




20 BUREAU OF GEOLOGY
Triassic Pangea reconstruction three microplates between North and South America, thus avoiding the overlap of the Bullard fit. During late Jurassic time, as North America split away from Europe, Africa, and South America, shear, with left-lateral sense of displacement, occurred along the transform faults that bounded the microplates. (from authors' abstract)
BALL, M. M. and C. G. A. HARRISON, 1969, Origin of the Gulf and Caribbean and implications regarding ocean ridge extension, migration, and shear: Gulf Coast Association of Geological Societies Transactions, vol. 19, p. 287-294.
The Gulf and Caribbean are a zone of north-south extension and left lateral shear opened between the Americas as these continents moved westward from Africa. The movements are related to ocean floor spreading away from the mid-Atlantic ridge. In order to accommodate spreading, the ridge itself migrates westward from Africa. Ridge migration is radial outward from Africa and results in opening triangular sheared grabens with apexes against Africa. A new ridge segment extends across these openings. Spreading rates vary and the migrating and extending ridge is sheared on fracture zones in response to these variations.
The currently popular related concepts of plate tectonics and transform faults are inconsistent with ridge migration and shear because these theories deny shear on fracture zones beyond ridge offsets and in the sense indicated by the position of ridge segments. Ridge migration and shear are a necessary complication of the spreading hypothesis. T-intersections of ridges are explained as intersections between a spreading and migrating ridge and a shear. The shear is only active on the side of the ridge toward which the migration is taking place. The junction of the mid-Atlantic ridge with the Azores-Gibraltar ridge is an example of such a feature. (authors' abstract)
BEALL, ROBERT, 1973, Plate tectonics and the origin of the Gulf Coast Basin: Gulf Coast Association of Geological Societies Transactions, vol. 23, pp. 109-114.
The origin of the Gulf Coast basin and many of the structures in the basin are explained by a proposed Gulf basin miniplate. The miniplate lies between a large right lateral megashear which extends from under'the eastern Gulf of Mexico to the east end of the Ouachita Mountains, and a left lateral megashear of similar proportions which parallels the Mexican coastline and extends to the Marathon uplift. The Llano uplift acted as a buttress against northwestward movement of the Gulf basin plate.
The plate is believed to have moved more than 400 miles to the northwest during a Precambrian-Paleozoic compression cycle. When compression ceased, at or near the end of the Paleozoic Era, the Mesozoic Gulf Coast basin was formed over the slowly tilting plate. Rebound, associated with the cessation of compression, caused tension faults to form along old zones of crustal weakness. The graben and other fault trends in and adjacent to the interior salt basins are believed to overlie these crustal




INFORMATION CIRCULAR NO. 98 21
faults as are some of the similar structural features of the coastal basin. (from author's abstract)
BEHRENDT, JOHN C., JOHN SCHLEE, JAMES M. ROBB, and KATHERINE M. SILVERSTEIN, 1974, Structure of the continental margin of Liberia, West Africa: Geological Society of America Bulletin, vol. 85, pp. 1143-1158.
Geophysical surveys made by RN/V Unitedgeo I (USGS-IDOE Cruise Leg 5), combined with earlier surveys and available geologic information, provide the basis for interpreting the structure of the continental margin of Liberia. This area lies at the junction of the Americas and Africa in published reconstructions of Gondwanaland prior to the opening of the North and South Atlantic in Jurassic and Cretaceous time, respectively.
Three fracture zones (St. Paul, Cape Palmas, and Grand Cess) are inferred in the area southeast of 90 30' W. on the basis of magnetic and gravity data, which is supported by bathymetric and seismic reflection data. The three fracture zones appear to exist as separate lineaments near the African coast. Farther seaward, they may be part of the same transform fault crossing the Atlantic (St. Paul fracture zone). The magnetic anomalies associated with these fracture zones, which may have originated in Cretaceous time at the opening of the South Atlantic, are continuous with magnetic anomalies over crust of Eburnean age (approx. 2,000 m.y.) in southeast Liberia and its continental shelf. This suggests that Eburnean age structures may have been zones of weakness that were reactivated in Cretaceous time.
A positive gravity anomaly (approx. 50 mgal) along the coast and continental shelf of Liberia is attributed to deep crustal rocks that were uplifted and exposed in Pan-African time (approx. 500 m.y.). The land boundary of this anomaly coincides with a shear zone that marks the boundary between the Pan-African and the Liberian age province (approx. 2,700 m.y.); the shearing (in a thrust-fault sense) may be the result of compressive stress associated with the closing of a proto-Atlantic ocean. Liberian age magnetic anomalies in the area northwest of 90 30' W. cross the Pan-African province (and the positive coastal gravity anomaly) and continue over the continental shelf and slope to about the 3,000 m bathymetric contour; the seaward limit of the anomalies is interpreted as representing the seaward limit of the old continental crust. This westward extension of the continental crust does not completely fill the gap in fit in various published reconstructions of Gondwanaland, and we suggest that the northern Florida block may have been located near the Liberian margin at one time.
Magnetic data indicate a thick section of sedimentary rock, possibly as great as 8 km, on the continental slope. Comparison of gravity data over magnetically inferred basins in the shelf, slope, and rise suggests that low-density sedimentary rocks constitute a greater proportion of the section in basins beneath the slope and rise northwest of 90 30' W. than beneath the slope and rise in the area of the fracture zones. The gravitational attraction




22 BUREAU OF GEOLOGY
that corresponds to a crust-mantle boundary dipping 450 to 600 can be computed to fit observed data-as might be expected at a rifted continental margin. A shallow high-density block beneath the coast and continental shelf is required to fit the coastal positive anomaly; this block is represented by exposures on land of granulite-grade metamorphic rock of the Pan-African province. (authors' abstract)
BUFFLER, RICHARD T., JOEL S. WATKINS, JEANNE F. SHAUB, and J. LAMAR WORZEL, 1980, Structure and early geologic history of the deep central Gulf of Mexico basin, in Pilger, R. H. (editor), The origin of the Gulf of Mexico and the early opening of the central North Atlantic Ocean:
Proceedings of a symposium, March 3-5, 1980, Louisiana State University, Baton Rouge, Louisiana, pp. 3-16.
Multifold seismic reflection data (27,000 km) and OBS refraction data collected recently by the University of Texas Marine Science Institute in the deep Gulf of Mexico provide the basis for a preliminary interpretation of the early (pre-middle Cretaceous) geologic history of the basin. The following observations can be made regarding the structure and stratigraphy of the deep central Gulf: 1) a thinned and rifted "transitional" crust (6-20 km thick) underlies the southern part of the deep central Gulf and extends up to 100 km seaward of the Campeche Escarpment; 2) the upper part of this transitional crust in places contains rift basins; 3) a major unconformity (strong, smooth reflector) truncates this transitional crust; 4) an oceanic crustal layer (5-6 km thick) underlies the rest of the central Gulf. The top of this layer corresponds to a strong irregular reflector seen on the seismic reflection data; 5) an outer basement high occurs along the boundary between oceanic crust and transitional crust; 6) a thick salt section overlies the transitional crust. It is bounded on the north and west by the outer basement high and pinches out depositionally to the south along the base of the Campeche Escarpment against the major unconformity (3 above). Salt appears to be absent or possibly very thin in the areas of oceanic crust; 7) there was an early period of deformation of salt and sedimentary rocks probably due to gravity flowage of the salt associated with the early rapid subsidence of the basin; 8) a younger undeformed sedimentary sequence onlaps the oceanic crust, the outer basement high and the deformed salt and sedimentary rocks. The upper part of this sequence probably represents the deepwater equivalent of the Lower Cretaceous carbonate banks that rimmed the early Gulf basin; 9) these older sedimentary sequences are truncated by a major regional unconformity that is tentatively correlated with a major middle Cretaceous (Cenomanian 97 m.y.) unconformity and drop in sea level.
The symmetrical distribution of transitional crust and thick salt on either side of oceanic crust as well as other data suggest that the Gulf basin evolved somewhat along the same lines as the North Atlantic, both as to timing and as to structure and stratigraphy. A model for the early evolution of the Gulf is proposed based on our interpretations and consists of four main phases as follows: a) a long period (Triassic-Early Jurassic) of




INFORMATION CIRCULAR NO. 98 23
regional uplift, doming, rifting, erosion and filling of rift basins with continental sediments and volcanics (Rift Phase). Formation of thinned continental crust or transitional crust; b) formation of a medial uplift due to mantle upwelling (Late Rift Phase). Initial subsidence, incursion of seawater and deposition of thick shallow-water evaporites in basins on either side of medial uplift (Middle Jurassic); c) a period of seafloor spreading in Late Jurassic-Early Cretaceous and formation of oceanic crust (Drift Phase). Rapid subsidence of the basin due to cooling of the crust. Deposition of deep-water sediments in the central Gulf and shallow-water sediments on adjacent margins overlying the salt. Early deformation due to gravity flowage of salt basinward; and d) abortion of seafloor spreading due to major plate reorganization about 130 m.y. ago. Continued subsidence of the basin through Lower Cretaceous as crust continues to cool (Subsidence Phase). Deposition of deep-water sediments across the deep basin and buildup of carbonate banks on the margins controlled by a structural hinge zone. Formation of a major middle Cretaceous (97 m.y.) unconformity due to a combination of a continued subsidence and a major drop in sea level. (authors' abstract)
DANIELS, DAVID L., ISADORE ZEITZ, and PETER POPENOE, 1983, Distribution of subsurface Lower Mesozoic rocks in the southeastern United States as interpreted from regional aeromagnetic and gravity maps, in Gohn, Gregory S. (editor), Studies related to the Charleston, South Carolina, earthquake of 1886-tectonics and seismicity: U. S. Geological Survey Professional Paper 1313-K, 24 p.
Aeromagnetic data, in conjunction with data from deep wells, are used to interpret the nature of the pre-Cretaceous "basement" beneath the Coastal Plain in Georgia and South Carolina. These data reveal some of the complexity of the broad early Mesozoic rift basin, which appears to extend at least from the Gulf of Mexico to the Atlantic Ocean. Along the northern edge of this rift, in the Savannah River region, depth-to-magnetic-source calculations delineate two interconnected basins, which are separated from the main rift by a broad horst of crystalline basement. The Riddleville (Ga.) basin appears to contain at least a 2.2-km thickness of basin fill; it is deeper than the Dunbarton (S. C.) basin, which has at least a 1.0 km thickness of fill. A maximum thickness of 3.5 km near Statesboro, Ga., is indicated for the main basin, called here the South Georgia rift.
Abundant lower Mesozoic diabase dikes in the South Carolina Coastal Plain are revealed on the magnetic map by narrow anomalies that have two dominant trends, northwest and north. One set of several north-trending anomalies can be traced continuously northward across the Coastal Plain, Piedmont, and Blue Ridge for 480 km. The two sets, which may represent two episodes of intrusion, have characteristic distributions within the study area: northwesterly trends are to the southwest and northerly trends to the northeast. A broad area of overlap extends from 800 W., in South Carolina, to northern Virgina. Several lower Mesozoic diabase sills within the rift are indicated by circular, low-amplitude magnetic anomalies.




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Intense magnetic highs and corresponding gravity highs indicate the presence of abundant large bodies of mafic rocks in the pre-Cretaceous "basement" in addition to the dikes and sills; two groups of mafic rocks are distinguished. Circular or oval anomalies are interpreted as largely gabbroic plutons, which may be as young as early Mesozoic and which are present both within and outside the rift. Elongate anomalies, which form a northeast-trending belt across Georgia and South Carolina, may reflect deformed pre-Mesozoic mafic rocks.
The largest and least understood magnetic feature of the region is the Brunswick anomaly, a long-wavelength anomaly system 1,100 km long, which is mostly offshore but which also bisects the Georgia Coastal Plain. The anomaly divides two regions of differing magnetic character and magnetic trend, which suggests that it is closely related to a Paleozoic suture between a Florida-South Georgia microcontinent and the North American craton. (authors' abstract)
DICKINSON, WILLIAM R., and PETER J. CONEY, 1980, Plate tectonic constraints on the origin of the Gulf of Mexico: in Pilger, R. H. (editor), The origin of the Gulf of Mexico and the early opening of the central North Atlantic Ocean: Proceedings of a symposium, March 3-5, 1980, Louisiana State University, Baton Rouge, Louisiana, pp. 27-36.
Drift history and plate interactions within the Caribbean region place severe constraints on hypotheses for the origin of the Gulf of Mexico. Various crustal elements of South America and Mesoamerica were sutured against North America when a Paleozoic ocean closed along the Ouachita segment of the Hercynian orogenic belt. Triassic positions for crustal blocks within Pangaea leave little or no space for a pre-Jurassic oceanic area in the region south of the North American craton. Lack of evidence for any Mesozoic or Cenozoic subduction around most margins of the present Gulf implies that the crustal blocks which separated during the Mesozoic to form the oceanic floor of the central Gulf were largely those that still rim the Gulf today. Prior to Jurassic opening of the Gulf, the Yucatan block including the Campeche bank thus nestled against the southern United States and eastern Mexico. Subsequent independent motion of Yucatan later in the Mesozoic was accommodated either by a northwesterly trending megashear that sliced through Mexico, or by a northerly trending transform that crossed thie present Isthmus of Tehuantepec. The positioning of Cuba across the mouth of the Gulf between Yucatan and Florida was accomplished by subduction along the northern flank of the Greater Antilles from medial Cretaceous to mid-Paleogene times. The western limit of the subduction zone was a transform or trans-tensional rift along the eastern edge of the Yucatan block. Northward motion of the greater Antilles relative to North America continued until collision of Cuba with the Bahama platform, whose crustal bulk effectively resisted subduction. Subsequent Neogene subduction of Atlantic lithosphere beneath the Caribbean plate has been confined to the Lesser Antilles arc-trench system. Coordinate Neogene transform slip along the north side of the Caribbean plate has




INFORMATION CIRCULAR NO. 98 25
opened the Cayman trough, and displaced nuclear Central America from its original Paleogene position south of the Sierra Madre del Sur. (authors' abstract)
DIETZ, ROBERT S., JOHN C. HOLDEN, and WALTER P. SPROLL, 1970, Geotectonic evolution and subsidence of Bahama Platform: Geological Society of America Bulletin, vol. 81, pp. 1915-1928.
The thick section (greater than 5 km) of flat-lying Cretaceous and younger carbonates capping the Bahama platform implies an unusual geotectonic history, characterized by great subsidence. We suggest that this platform is underlain neither by sial nor by a volcanic foundation creating a "mega-atoll." Instead we propose a basement of oceanic crust about 11 km down which has undergone slow subsidence. Triassic rifting in the Atlantic probably initially created a closed small ocean basin, or mediterranean, in the Bahama region. This was accomplished by a rotational movement of the North American plate away from North Africa accompanied by shearing across the top of the South American plate which remained stationary and attached to Africa. A wedge-shaped sphenochasm resulted which became a sediment trap within Pangaea and quickly filled to sea level with turbidites. With renewed continental drift, the Bahama platform became a subsiding marginal plateau attached to the North American craton upon which algal-coral growth exposively flourished under holo-oceanic conditions, providing sufficient upbuilding to offset subsidence and maintain a sea level freeboard.
This interpretation obviates the overlap of the Bahama salient onto the African craton when the Atlantic Ocean is closed under continental drift reconstruction. It accounts for the long history of subsidence without calling on "oceanization." It also explains the inference, based on some Cuban-Soviet geophysical evidence, that there is a thick sedimentary section beneath the Bahamian carbonates. An underlying clastic sequence could also include the source of the probable salt domes at the bottom of Exuma Sound. (authors' abstract)
Note that, as the authors point out in their development of the model, although the discussion is primarily restricted to the Bahama platform, the explanation could possibly include contiguous geologically similar regions, i.e., the southern one-fourth of Florida and a portion of the Blake marginal plateau. Also, as discussed in the conclusion of the paper, if the inferred Lower Mesozoic clastic section is verified, it should offer good oil and gas prospects with deep drilling.
DILLON, WILLIAM P., and CHARLES K. PAUL, 1982, Summary of development of the continental margin off Georgia based on multichannel and single-channel seismic-reflection profiling and stratigraphic well data:
in Arden, Daniel P., Barry F. Beck, and Eleanor Morrow, (editors), Proceedings of the second symposium on the geology of the Southeastern Coastal Plain: Americus, Georgia, March 5-6, 1979, Georgia Geological Survey Information Circular 53, pp. 197-200.




26 BUREAU OF GEOLOGY
The U. S. Geological Survey has collected a grid of 9,000 km of deep penetration, common-depth-point, seismic reflection profiles on the U. S. southeastern continental margin in order to study the structure, development, and petroleum potential of the region. Profile TD-5 extends from the outer part of the Southeast Georgia Embayment, across the northern end of the Blake Plateau basin, and eastward to the deep sea. It passes through three deep drill sites which provide stratigraphic control. Along with knowledge gained from the remainder of the grid, profile TD-5 is used to characterize the development of the continental margin off Georgia. A summary of this development is given by the authors:
"The continental margin off Georgia probably began to form with rifting, mafic intrusive and extrusive activity, and rapid sediment deposition which led to development of a transitional basement.
Early subsidence was rapid for the basement beneath the present Blake Plateau basin, and the Upper Jurassic deposits form the thickest unit. Reefs acted as sediment dams at the seaward side of the basin. Near the end of the Neocomian, the reefs died, but a new reef formed slightly to landward and continued to form a sediment dam until the end of the Early Cretaceous. Subsequently, the Blake Plateau has been a moderately deep water environment (several hundred meters) until present. The Gulf Stream became significant on the Blake Plateau near the Paleocene-Eocene boundary, and since then has prevented the
shelf sediments from prograding across the plateau."
DILLON, WILLIAM P. and JEAN M. A. SOUGY, 1974, Geology of West Africa and Canary and Cape Verde Islands: in, Nairn, Alan E. M. and Francis G. Stehli, (editors), The ocean basins and margins; Volume 2, The North Atlantic: Plenum Press, New York, pp. 315-390.
Research and study of the geotectonic history of the Florida basement requires familiarity with West African geology. This paper is an excellent reference work on West African geology. It includes detailed descriptions of the structural framework and geologic history, from Precambrian to Quaternary, of West Africa and the Canary and Cape Verde Islands.
DRAKE, C. L., J. HEIRTZLER, and J. HIRSHMAN, 1963, Magnetic anomalies off eastern North America: Journal of Geophysical Research, vol. 68, pp. 5259-5274.
Numerous magnetic profiles have been made across the continental margin of eastern North America by the U. S. Geological Survey, the U. S. Navy Hydrographic Office, and the Lamont Geological Observatory. These data, supplemented by areal studies in parts of the region, reveal an anomaly pattern which is essentially parallel to the margin and to the major structural features on shore. Calculations show that, while basement topography may contribute, the principal causes of the anomalies are compositional changes within the basement. Two exceptions to the pattern are noted; one is southern Florida, suggested by E. R. King (1959) to be an




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extension of the Ouachita system, and the other is a major feature normal to the coast at latitude 400 N interpreted as being associated with a transcurrent fault. Other geophysical and geological observations indicate a right lateral displacement of the fault of about 100 miles and a total length in excess of 600 miles. The implications of this and the possibility of other transcurrent movements along the Atlantic margin are examined. (authors' abstract)
FREELAND, GEORGE L., and ROBERTS. DIETZ, 1971, Plate tectonic evolution of Caribbean-Gulf of Mexico region: Nature, vol. 232, pp. 20-23.
A geotectonic model for the evolution of the "American Mediterranean" (Caribbean-Gulf of Mexico region) is presented. Microcontinents, which are later translated, eliminate the overlaps and oceanic areas in the Paleozoic reconstruction of the region by Bullard et al. (1965). Areas underlain by pre-Mesozoic basement are included in the microcontinents; neo-cratons (i.e. "new ground" created during Mesozoic-Cenozoic time) are eliminated. The microcontinents included Oaxaca (southern Mexico), Yucatan, Honduras-Nicaragua, and southeastern Bahama platform (the nature of the Blake-Florida-Bahama platform basement is still unknown; for this reconstruction it is assumed to be pre-Mesozoic). The evolution of the Caribbean-Gulf of Mexico region, including the rotation and translation of these microcontinents, as related to the tectonic motions of the North American, South American, and African plates, is shown in seven time-sequence reconstructions from Paleozoic to present.
HALL, D. J., T. D. CAVANAUGH, J. S. WATKINS, and K. J. McMILLEN, 1982, The rotational origin of the Gulf of Mexico based on regional gravity data: in Watkins, J. S. and C. L. Drake (editors), Studies in continental margin geology: American Association of Petroleum Geologists Memoir 34, pp. 115-126.
Regional free-air gravity data from the Gulf of Mexico define deep-seated linear features which we interpret as outer marginal basement highs. Highs are arranged symmetrically around the deep water Gulf. Abrupt changes in trend occur along three well-defined zones on both sides of the central Gulf. The marginal high off Galveston parallels the Cretaceous Edwards Reef trend 230 km to the northwest. We interpret the seaward limits of these outer marginal highs as close to the landward edges of oceanic crust. The crust in the area from the continental hinge zone (near which the Edwards Reef developed) to the outer high is thinned, faulted, and intruded by mafic dikes, but probably has a nearly continental overall composition.
We infer that the Gulf opening followed a pattern of early rifting and subsequent sea-floor spreading. Our model implies that the thick salt deposits underlying the modern Texas slope were deposited on sediments overlying oceanic crust. Thinner salt deposits overlie pre-salt sediments on rift-stage crust both northwest of the Texas outer marginal high and in the Sigsbee Knolls. A change in the location ofthe sea-floor spreading center




28 BUREAU OF GEOLOGY
led to separation of the two main salt depo-centers beneath the Sigsbee Knolls and along the Texas-Louisiana shelf and slope. Recent paleomagnetic evidence (L. Sanchez Barreda, personal communication, 1981) indicates a post-Permian, 240 clockwise rotation of Chiapas relative to Oaxaca (this is consistent with our rotational model). The Salina Cruz fault, crossing the Isthmus of Tehuantepec between the Permian outcrops in Chiapas and Oaxaca, was probably a major transform fault active during the Gulf opening. (authors' abstract)
HORTON, J. WRIGHT, JR., ISIDORE ZIETZ, and THORTON L. NEATHERY, 1984, Truncation of the Appalachian Piedmont beneath the Coastal Plain of Alabama: Evidence from new magnetic data: Geology, vol. 12, pp. 51-55.
A new aeromagnetic survey of a part of southern Alabama reveals that magnetic signatures of the Appalachian Piedmont are truncated by a major magnetic lineament beneath the Gulf Coastal Plain. Mylonitic rocks have been recovered from a drillhole along this lineament, which is probably a fault zone of late Paleozoic and/or Triassic-Jurassic age. We suggest that this fault zone may initially have been the Alleghanian convergent suture between the North American craton and accreted terranes to the southeast. The zone may have been locally reactivated as part of an extensive buried Triassic-Jurassic graben system. (authors' abstract)
IBRAHIM, ABOU-BAKR K., J. CARYE, G. LATHAM, and RICHARD T. BUFFLER, 1981, Crustal structure in Gulf of Mexico from OBS refraction and multichannel reflection data: American Association of Petroleum Geologists Bulletin, vol. 65, pp. 1207-1229.
Results from 12 reversed refraction profiles each 110 km long have been combined with multichannel reflection data to produce a series of crustal structure sections across the Gulf of Mexico. These data show as many as three layers of sedimentary rocks with total thickness between 5 and 9 km and layer velocities between 1.7 and 3.5 km/sec. Beneath most of the Gulf, this sedimentary section is underlain by a layer with velocity between 4.5 and 5.5 km/sec. The acoustic basement as defined by reflection data is confined within this layer. Beneath this layer in most of the deep Gulf is an oceanic crustal layer, 3 to 6 km thick which thickens to about 12 Km under the Mississippi fan and 10 km in the southeastern Gulf where it is interpreted to be transitional crust. This layer has a velocity between 6.4 and 7.0 km/sec and overlies a mantle with velocity between 7.6 and 8.2 km/sec.
These data confirm earlier refraction interpretation that most of the deep Gulf basin is underlain by an oceanic crustal layer flanked by transitional crust. This layer may have been formed by a mantle thermal event accompanied by a period of rapid sea-floor spreading. (from authors' abstract)
IBRAHIM, ABOU-BAKR K. and ELAZAR UCHUPI, 1982, Continental




INFORMATION CIRCULAR NO. 98 29
oceanic crustal transition in the Gulf Coast geosyncline: in, Watkins, J. S. and C. L. Drake (editors), Studies in continental margin geology: American Association of Petroleum Geologists Memoir 34, pp. 155-165.
Seismic refraction measurements indicate that the transition from rifted continental crust to oceanic crust takes pace at a water depth of over 3000 m northwest of Cuba between the Florida and Campeche escarpments. Along the eastern flank of the Mississippi Embayment, the transition occurs at about 2500 m deep and on the embayment itself inboard of the coast. Off south Texas the boundary between the rifted continental crust and oceanic crust is near the shelf's edge, off Mexico the boundary is on the continental slope, and off Campeche Bank the boundary is about 100 km northwest of Campeche Escarpment. In the northern Gulf an oceanic crustal high may lie beneath the upper continental slope. This high served as a foundation for a Mesozoic reef. Maximum sediment accumulation took place along the contact between the rifted continental crust and oceanic crust. (authors' abstract)
KLITGORD, KIM D., WILLIAM P. DILLON, and PETER POPENOE, 1983, Mesozoic tectonics of the southeastern United States Coastal Plain and continental margin: in Gohn, Gregory S. (editor), Studies related to the Charleston, South Carolina, earthquake of 1886-tectonics and seismicity:
U. S. Geological Survey Professional Paper 1313-P, 15p.
Many of the major structures associated with Paleozoic and Mesozoic tectonic events along the Southeastern U. S. Coastal Plain and continental margin have distinctive geophysical and geological properties, which are described in this integrated study of magnetic, gravity, seismic-reflection, and drill-hole data. These data are used to identify three major tectonic boundaries that separate terranes of Paleozoic, Triassaic, and Jurassic tectonic activity and to map sedimentary basins that were formed by Triassic and Jurassic rifting events. The major tectonic boundaries are: (1) An offshore hinge zone in basement that separates an area of crustal subsidence associated with the Jurassic-age marginal basins from an area of significantly less subsidence associated with Triassic and older basement structures to the west; (2) a line of narrow grabens, associated with the magnetic low in the Brunswick magnetic anomaly, that separates a Paleozoic basin underlying northeastern Florida, which was not greatly affected by late Paleozoic or Triassic tectonic activity, from a broad zone of considerable Triassic tectonic activity and sediment accumulation in the Charleston, S. C., region; and (3) a narrow east-west zone near 330 N that separates the geophysically distinctive northeast-trending Piedmont to the north from the Charleston region. The Triassic sedimentary basins are of two types: (1) narrow basins or grabens within the Piedmont and along the major tectonic boundaries and (2) broad zones of sediment accumulation over a block-faulted Paleozoic basin in northwestern Florida and in areas delineated by low-gradient magnetic and gravity fields in parts of the Charleston region. Deep continental margin basins, containing sedimentary rock as much as 14 km thick, formed at sites of Jurassic rifting and




30 BUREAU OF GEOLOGY
subsequent ocean opening seaward of the basement hinge zone. Reconstruction of the positions of the North American, South American, and African continents during the Early Jurassic provides a framework for relating the Mesozoic tectonic events and structures to major Paleozoic orogenic events and lithotectonic units. (authors' abstract)
LADD, JOHN W., 1976, Relative motion of South America with respect to North America and Caribbean tectonics: Geological Society of America Bulletin, vol. 87, pp. 969-976.
Magnetic anomalies in the North Atlantic have been analyzed by Pitman and Talwani (1972) to determine a sequence of finite difference poles of relative motion of North America with respect to Africa for the time period 180 m.y. B.P. to the present. A similar analysis of South Atlantic magnetic anomalies by the writer determines a sequence of finite difference rotations of South America with respect to Africa for the time period 127 m.y. B.P. to the present. The two sequences of finite difference rotations are used to calculate the relative motion of South America with respect to North America for late Mesozoic and Cenozoic time.
From Triassic to Early Cretaceous time, South America moved to the southeast away from North America. From Early Cretaceous to Late Cretaceous time, South Amerca moved eastward with respect to North America. Southeastward motion of South America occurred again from Late Cretaceous to early Tertiary time followed by northward motion from early to late Tertiary. Tectonic styles in the Caribbean region change when major plate motions change; however, the details of Caribbean geology cannot be explained by simple plate margins between North and South America. Tertiary compressional structures on the northern and southern margins of the Caribbean can be attributed to Tertiary closure between North and South America, but earlier tectonic regimes are not so easily related directly to North America-South America motions. (authors' abstract)
MULLINS, HENRY, T., and GEORGE W. LYNTS, 1977, Origin of the northwestern Bahama Platform: Review and reinterpretation: Geological Society of America Bulletin, vol. 88, pp. 1447-1461.
The origin of the Bahama Platform has been the subject of debate for more than a century. The major points of disagreement are (1) whether the Bahamian basement is continental or oceanic, and (2) the age and origin of the deep Bahama channels. Geophysical data indicate only that the Bahamian basement is of intermediate density, seismic velocity, and thickness. We propose that this basement was originally pre-Triassic continental material that was pervasively intruded by mafic and ultramafic material during the rifting of North America from Africa and South America in Late Triassic time. To alleviate the Bahama overlap in reconstructions of the North Atlantic we suggest that the Bahama Platform has been rotated approximately 25* to the northeast by the relative impinging motion of the Caribbean plate during Cretaceous and early Tertiary time. By accounting




INFORMATION CIRCULAR NO. 98 31
for this postulated rotation, the Bahama Platform forms an excellent fit between Africa and South America.
We propose the following model for the origin of the northwestern Bahama Platform: (1) The platform is continental and was originally part of Africa. (2) Rifting of North America from Africa and South America began in the vicinity of the northwestern Bahamas during the Late Triassic, preceded by a large domal uplift of the continents that initiated the deep Bahama Channels as grabens. (3) The Bahama Platform rifted from Africa principally along a large right-lateral shear and thus evolved as a transcurrent-type continental margin. (4) During the incipient development of the deep Bahama channels, Late Triassic continental arkosic rudites and arenites were deposited at the base of these grabens; (5) Initial marine conditions in Early to Middle Jurassic time may have resulted in the deposition of salt and organic-rich shales in the channels due to restricted circulation. (6) With the onset of more open marine conditions 3 to 6 km of Jurassic to Holocene deep-water carbonate and bioclastic turbidite sediments were deposited in the channels. (7) Most of the intraplatform relief of the northwestern Bahamas appears to be the result of the build-up of the banks relative to the channels during regional subsidence. (authors' abstract)
PILGER, REX H., JR., 1978, A closed Gulf of Mexico, pre-Atlantic Ocean plate reconstruction and the early rift history of the Gulf and North Atlantic:
Gulf Coast Association of Geological Societies Transactions, vol. 28, pp. 385-393.
Several diverse lines of evidence indicate that the pre-Gulf of Mexico position of South America was adjacent to the northern Gulf Coast of North America in earliest Mesozoic time, as originally suggested by Walper and Rowett (1972). These include: 1) correlation of the boundary between Hercynian and pre-Hercynian terranes in Africa with the subsurface boundary between the southern Appalachians and the Florida platform in North America, 2) similarities in the inferred Triassic history of the Gulf and Atlantic coasts of North America; 3) recognition of significant left-lateral faulting in Mexico and Central America, which indicates more westerly positions of the various crustal blocks of Middle America prior to initiation of drift and, consequently, eliminates overlap of South America and Mexico of other reconstructions; 4) accommodation of the Florida-Bahama platform (assumed to be continental) by subsequent crustal extension and left-lateral faulting; 5) accommodation of Atlantic coast-Africa overlaps by crustal extension reflected in the on and offshore Triassic basins, and 6) satisfaction of paleomagnetic data which seem to require more northerly positions of the Gondwana continents relative to the Laurasian continents in latest Paleozoic and earliest Mesozoic time.
The post-rifting history inferred from the reconstructions and other constraints suggests the Gulf began opening in a north-south direction in early Mesozoic time, while right-lateral, obliquely divergent movement was occurring along the Atlantic coast between Africa and North America. Such




32 BUREAU OF GEOLOGY
motion was accommodated in part by formation of the Triassic rift basins. Subsequently, in late Triassic time, Africa and South America began moving in a southeasterly direction relative to North America. During this period, and into the early Jurassic, the Florida-Bahama platform was extended and emplaced along left-lateral faults roughly parallel to the direction of plate motion. Eastward motion of Mexico and Central America along left-lateral faults continued with opening of the Gulf of Campeche in Jurassic time, and movement of the various crustal fragments of Middle America into the Caribbean region during the Cretaceous and early Cenozoic. Contemporary east-west left-lateral movement is occurring along the plate boundary separating the North American and Caribbean plates.
These inferences suggest that the Gulf of Mexico is older than the Atlantic, and is underlain by the oldest oceanic crust still preserved in the world ocean basins. Further, it is likely that initial fragmentation of Gondwana from Laurasia involved a large component of strike-slip motion, concentrated along the axes of the older Appalachian-Hercynian mountain belts. (author's abstract)
SHERIDAN, ROBERT E., and WILLIAM L. OSBURN, 1975, Marine geophysical studies of the Florida-Blake Plateau-Bahamas Area: in Yorath, C. J., E. R. Parker and D. J. Glass, (editors), Canada's continental margins and offshore petroleum exploration: Canadian Society of Petroleum Geologists Memoir 4, pp. 9-33.
Marine seismic refraction and reflection profiles correlated with deep wells on land reveal that the Blake Plateau is underlain by 7-11 km of Jurassic and younger carbonates and evaporites, with some terriginous sediments. Rock dredges and cores show that the area is bordered by an apparently continuous reefal complex of Cretaceous and earlier age which extends from the Blake Escarpment through the Bahamas and Cuba to the West Florida Escarpment. JOIDES drilling on the Blake Plateau indicates that the Tertiary sedimentary section is abbreviated due to the erosional sweeping of the Gulf Stream. JOIDES Deep Sea Driling Project results and more recent piston coring reveal a complex Cenozoic history of hemipelagic and turbidite deposition in the Blake-Bahama Basin and on the Blake Outer Ridge. Contour currents apparently built the Outer Ridge then shifted deposition west of the ridge into the basin in the Late Miocene.
The origin of the basement under the Blake Plateau and Bahamas is still unknown from direct evidence. Indirect geophysical evidence, including magnetic anomalies, and Rayleigh Wave dispersion data, suggest the possibility that the basement is about 10 km deep and of intermediate density and seismic velocity. Such a crust might be correlated with that of the present Red Sea, and the Blake Plateau-Bahamas crust could be interpreted to have formed in a similar way in the Jurassic, or possibly the Triassic, as North America and Africa rifted apart. Basement faulting associated with the rifting and plate rotation of North America controlled the




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formation and subsidence of the deep geosynclinal basin under the Blake Plateau.
Porous dolomite horizons and cavernous reefal limestone are known in the area. Regional dip caused by differential subsidence of compaction over reefs, faults affecting Cretaceous and older strata, and possible salt doming might offer entrapment situations for these existing reservoirs. Golden Lane analogies and Smackover continuations are possible and stratigraphic traps are very probable. The potential for large petroleum reserves is real but their exploration and exploitation will be difficult. (authors' abstract)
TANNER, WILLIAM F., 1965, The origin of the Gulf of Mexico: Gulf Coast Association of Geological Societies, Transactions, vol. 15, pp. 41-44.
The Gulf of Mexico dates from approximately the Paleozoic-Mesozoic time boundary. From structural considerations, the hypothesis is developed that the present Gulf is the result of a slowly-widening rift, or tension gap, between North America and Central America and the Caribbean block. A general program of investigations, designed to test or at least explore the hypothesis, is outlined. (from author's abstract)
TODD, R. G., and R. M. MITHCUM, JR., 1975, Seismic stratigraphic identification of eustatic cycles in Late Triassic, Jurassic, and Early Cretaceous rocks, Gulf of Mexico and West Africa: Gulf Coast Association of Geological Societies Transactions, vol. 25, pp. 41-43.
Seismic stratigraphic techniques permit identification of Late Triassic, Jurassic, and Early Cretaceous eustatically controlled sequences in strata from the North American Gulf Coast and West Africa. Several distinct sequences are remarkably persistent from the Florida panhandle around the perimeter of the Gulf Coast into northern Mexico, a distance of over 1,500 miles. Their identification requires the integration of seismic data with lithologic, environmental-facies, biostratigraphic, radiometric, and well log information. A comparison with strata of comparable age in offshore West Africa are interpreted to be eustatically controlled because they occupy the same time-stratigraphic positions and display coastal onlap patterns similar to those previously recognized by us elsewhere in the world. (from authors' abstract)
VAN DER VOO, R., F. J. MAUK, and R. B. FRENCH, 1976, Permian-Triassic continental configurations and the origin of the Gulf of Mexico: Geology, vol. 4, pp. 177-180.
Previously published reconstructions of Pangea during the late Paleozoic-early Mesozoic time have suggested that (1) the Gulf of Mexico has existed as an oceanic basin from at least the late Carboniferous onward or (2) the Gulf of Mexico was created since Permian time by a process of microplate reorganization, macroplate drift, or oceanization (sensu stricto). On the basis of paleomagnetic data, we favor macroplate drift. Major geologic and tectonic features of the Pangea segments bordering the Gulf




34 BUREAU OF GEOLOGY
of Mexico are in agreement with a newly proposed alternative fit of North America, Europe, and Gondwanaland for late Paleozoic time. This reconstruction closes the Gulf of Mexico by juxtaposition of North and South America. (authors' abstract)
WALPER, JACK L., 1980, Tectonic evolution of the Gulf of Mexico: in Pilger, R. H. (editor), The origin of the Gulf of Mexico and the early opening of the central North Atlantic Ocean: Proceedings of a symposium, March 3-5, 1980, Louisiana State University, Baton Rouge, Louisiana, pp. 87-98.
A modification, by Walper and Rowett (1972), of the Paleozoic reconstruction of Pangea by Bullard et al. (1965) closed the Gulf of Mexico and placed Mexico and Central America adjacent to northwestern South America. Further modification of this reconstruction adds another three degrees of rotation to the 20-degree clockwise rotation of Gondwanaland proposed by Van der Voo et al. (1976). While this does not significantly affect the alignment of the pre-Mesozoic orogenic belts of West Africa and North America, it greatly improves the fit of North and South America. It also provides a better explanation of late Paleozoic history and the initiation of rifting that formed the Gulf of Mexico and Caribbean. This history of the Gulf of Mexico-Caribbean region is given in the author's abstract as follows:
"As the Late Pennsylvanian collision of the Afro-South American plate with the North American formed Pangea, convergence with a Pacific plate produced a Permo-Triassic arc-trench system along much of western North America. It remained active as North America moved away from a Triassic spreading ridge that passed from the Pacific into the Gulf and beyond into the North Atlantic, creating a narrow seaway similar to the Red Sea, in which thick salt deposits accumulated. As spreading continued and this sea widened, a Scotia-like arc developed between the diverging North and South American plates. The Gulf of Mexico evolved on the trailing margin of the North American plate while the Caribbean grew from the arc segment as North and South America diverged and the spreading ridge shifted from the Caribbean to the South Atlantic. Laramide tectonism, the result of continued convergence with a Pacific plate, transported Mexico eastward, initiating events that displaced part of the salt basin and changed the Gulf of Mexico from a normal trailing plate margin to a vast sediment trap for Cenozoic erosional debris derived from rejuvenated hinterland
sources."
WALPER, J. J., F. H. HENK, JR., E. J. LOUDON, and S. N. RASCHILLA, 1979, Sedimentation on a trailing plate margin: the northern Gulf of Mexico: Gulf Coast Association of Geological Societies Transactions, vol. 29, pp. 188-201.
The breakup of Pangaea and the splitting of South America from North America in the early Mesozoic left a rifted and attenuated trailing margin on the latter plate which became the initial depositional surface for a




INFORMATION CIRCULAR NO. 98 35
sedimentary sequence of Late Triassic to Recent age. The Late Triassic Eagle Mills Formation and its equivalents are Interpreted as being the initial deposits confined to rift grabens of the attenuated plate margin. Deposition of Jurassic evaporites resulted from sedimentation by the brine mixing process In the restricted circulation of a young and narrow seaway similar to the Red Sea. Late Jurassic and Cretaceous strata represent the transgressive deposits formed as open marine conditions prevailed as the plates diverged and the North American plate margin subsided. Laramide tectonism in the continental Interior provided a rejuvenated hinterland source area that supplied the voluminous sediment for the regressive and prograding Cenozoic clastic wedge.
Studies of this entire sedimentary record reveal the Influence of the tensional effects of continental splitting and lower crustal creep that established the initial depositional surface that slowly subsided as indicated by crustal thinning and the thermal decay curve of cooling oceanic lithosphere. In addition, these studies also reveal the control and influence of: 1) inherited structures of the rifted margin; 2) hinterland source area; 3) the timing and amount of differential subsidence between continental and ocean crust; 4) active syndepositional faults; 5) hingelines; and 6) post depositional rejuvenation due to contemporary plate movement.
Not only do these studies add to our understanding of the geologic history of the area, which is most important for development of successful exploration programs, but they provide a guide for the study of sedimentary infills within ancient lithospheric plates, a neglected but important task facing all who are confronted by the complex problem of interpreting the sedimentary record of ancient basins. (authors' abstract)
WALPER, JACK L., and C. L. ROWETT, 1972, Plate tectonics and the origin of the Caribbean Sea and the Gulf of Mexico: Gulf Coast Association of Geological Societies Transactions, vol. 22, pp. 105-116.
Previously published reconstructions of the late Paleozoic "fit" of crustal plates and continents fail to explain many geological features present in southwestern United States, Mexico, Central America and northern South America. In particular, they fall to consider major geologic and tectonic continuities of Paleozoic age observable in the Southern Appalachians, the Ouachita and Marathon fold belts, the fold belts of southern Mexico and Central America, and the eastern Andean Mountain belt of northern South America, as well as the significance of a number of major transcurrent fault systems or megashears that cross these regions.
With the well documented Africa-North America join as a control for the positioning of South America relative to North America, this report suggests a somewhat different "fit" than any heretofore proposed. Instead of truncating North America in northern Mexico and filling in the Gulf of Mexico with fragments as is most commonly done, this reconstruction wraps Mexico and Central America around the western margin of South America, thus placing in juxtaposition the major tectonic belts of both continents. Evidence is also presented indicating that the late Ordovician Taconic




36 BUREAU OF GEOLOGY
orogeny was an arc-continent collision rather than a continent-continent collision as has previously been suggested. Similar evidence indicates that the late Paleozoic Ouachita and Marathon orogenies were arc-continent collisions. Correlative periods of deformation for both of these orogenies have been documented from many places in northern and northwestern South America.
The early Paleozoic history of the Cordilleran mobile belt appears to have been independent from that of the eastern mobile belt. In the late Paleozoic, however, these mobile belts seem to have become tectonically coupled to produce regional stresses that were released along several major megashears. In southern and southwestern North America these include the Wichita and Texas megashears; a third megashear is probably present in northern Mexico. Late Paleozoic movement is probably present in northern Mexico. Late Paleozoic movement on these fault zones produced numerous basins and uplifts throughout all of these regions.
Modifications of the model proposed by Malfait and Dinkelman (1972) for the origin of the Caribbean region are proposed that include the opening of a sphenochasm in the Gulf of Honduras and regional tensional and compressional stresses resulting from the clockwise rotation of North America. The Gulf of Mexico and the present dislocated positions of the Ouachita and Marathon fold belts are explained as the result of an opening sphenochasm under the present Mississippi embayment and the westward displacement of the Ouachita and Marathon fold belts by left lateral movement on the Wichita and Texas megashears. (authors' abstract)
WILSON, J. TUZO, 1966, Did the Atlantic close and then reopen?: Nature, vol. 211, pp. 676-681.
Paleontologic, structural, tectonic, and geometric evidence is presented for the hypothesis that, in the Paleozoic, an existing proto-Atlantic Ocean closed and that, in the Cretaceous, the present Atlantic Ocean opened. In Early Paleozoic time, the proto-Atlantic formed the boundary between two distinct faunal realms. During Middle and Late Paleozoic time this ocean closed by stages, bringing the dissimilar realms together. Available geological evidence suggests that the present Atlantic Ocean started opening at the beginning of the Cretaceous. The opening occurred along a different line than the earlier closing. Fragments of the continents which were brought together during Middle and Late Paleozoic time thus traded sides when the present Atlantic opened during the Cretaceous. This resulted in some regions of similar faunas being separated by the Atlantic while other regions of dissimilar faunas became adjacent to one another.
WOOD, MICHAEL L., and JACK L. WALPER, 1974, The evolution of the Interior Mesozoic Basin and the Gulf of Mexico: Gulf Coast Association of Geological Societies Transactions, vol. 24, pp. 31-41.
The evolution of the Interior Mesozoic Basin is presented in terms of an evolving Gulf of Mexico which had its origin with the rifting and breakup of Pangea, particularly with the separation of North and South America. This




INFORMATION CIRCULAR NO. 98 37
Mesozoic event was preceded by the formation of Pangea in the late Paleozoic when plate collision produced the Appalachian-Ouachita-Marathon orogeny. As a result of this orogenic episode of plate collision and accompanying crustal dislocation along three major transcurrent fault systems, the Texas, Wichita and Mississippi megashears, a proto-Atlantic was closed and a distributive pattern of pre-Mesozoic rocks was created that was to have a lasting effect on the shape of the Interior Mesozoic Basin.
Rifting in the early Triassic created an incipient Gulf of Mexico with associated peripheral grabens that defined the shape of Mesozoic sedimentation. Crustal thinning and attenuation accompanied the divergent rifting of Pangea and early sedimentation in rift grabens is represented by the Eagle Mills Formation. Deltaic prisms are postulated, coincident with the three megashears, and represent the positions of ancestral Rio Grande, Red and Mississippi Rivers. They augment the continental red beds of the grabens formed during early rifting and the succeeding marine shelf sediments of a diverging plate margin and constitute exploratory objectives.
The thick evaporite deposition, represented by the Werner Evaporite and Louann Salt, in a shallow basin on a subsiding plate margin is the result of an unique combination of events. The updomed rift margin of the trailing plate formed a restricting barrier that allowed the continued influx of sea water into the attenuated and rifted portion of the plate that was subsiding to form the Interior Mesozoic Basin. The sea water, upon encountering the highly saline waters of this subsiding basin initiated rapid salt deposition by the brine mixing method. Eastward rotation of Mexico into its present position deepened the Gulf of Mexico and peripheral rifting aided in continued submergence with normal marine deposition being established in late Jurassic time. (authors' abstract)
WOODS, R. D., and J. W. ADDINGTON, 1973, Pre-Jurassic geologic framework, Northern Gulf Basin: Gulf Coast Association of Geological Societies Transactions, vol. 23, pp. 92-108.
Early history of the Gulf basin is conjectural. It was once believed the basin formed by late Paleozoic foundering of Llanoria, a postulated large offshore landmass occupying much of the present basin area. Currently, there are two schools of thought: (1) the basin has existed since late Precambrian; (2) it was formed by early Mesozoic seafloor spreading in the Gulf, a product of the general breakup of old Pangaea into continental blocks.
Upper Paleozoic orogeny, in phase with or a part of a west-southwestward continuation of Appalachian folding, created a northern structural rim for the basin which strongly influenced subsequent sedimentation and structural trends. Post-orogenic tension faulting along and south of this rim was particularly active during the Triassic. Jurassic sediments along the flank and gulfward from the structural rim overlie this faulted basin floor and are in unconformable contact with rocks ranging in age from Triassic to Mississippian.
Triassic sediments are fluvial to deltaic red beds. Paleozoic deposits




38 BUREAU OF GEOLOGY
include both "Ouachita facies" and unmetamorphosed fluvial to offshore marine clastic and highly fossiliferous shallow water carbonates. Seismic data suggest Traissic and/or late Paleozoic sediments underlie Jurassic throughout the Gulf Basin. These pre-Jurassic rocks comprise a large, very sparsely tested frontier for oil and gas. (authors' abstract)




INFORMATION CIRCULAR NO. 98 39
REFERENCES
(This is a list of references cited within the bibliography.)
Anderson, Thomas H., and Victor A. Schmidt, 1983, The evolution of Middle America and the Gulf of Mexico-Caribbean Sea during Mesozoic time: Geological Society of America Bulletin, vol. 94, pp. 941-966.
Bullard, E., J. E. Everett, and A. G. Smith, 1965, The fit of the continents around the Atlantic: in Symposium on continental drift: Royal Society of London Philosophical Transactions, series A, vol. 258, no. 1088, pp. 41-51.
Dietz, Robert S., John C. Holden, and Walter P. Sproll, 1970, Geotectonic evolution and subsidence of Bahama Platform: Geological Society of America Bulletin, vol. 81, pp. 1915-1928.
Dillon, William P., and Jean M. A. Sougy, 1974, Geologyof West Africa and Canary and Cape Verde Islands: in Nairn, Alan E. M. and Francis G. Stehli (editors), The ocean basins and margins; vol. 2, The North Atlantic: Plenum Press, New York, pp. 315-390.
Freeland, George L., and Robert S. Dietz, 1972, Plate tectonic evolution of the Caribbean-Gulf of Mexico Region: Proceedings of the sixth Caribbean Geological Conference, pp. 259-264.
King, Elizabeth R., 1959, Regional magnetic map of Florida: American Association of Petroleum Geologists Bulletin, vol. 43, pp. 2844-2854.
LePichon, X. J. C. Sibuet, and J. Francheteau, 1977, The fit of the continents around the North Atlantic Ocean: Tectonophysics, vol. 38, pp. 169-209.
Malfait, Bruce T., and Menno G. Dinkelman, 1972, Circum-Caribbean tectonic and igneous activity and the evolution of the Caribbean plate:
Geological Society of America Bulletin, vol. 83, pp. 251-272.
Pitman, Walter C., 111, and Manik Talwani, 1972, Sea-floor spreading in the North Atlantic: Geological Society of America Bulletin, vol. 83, pp. 619-646.
Talwani, M., J. L. Worzel, and M. Landisman, 1959, Rapid gravity computations for two-dimensional bodies with application to the Mendocino submarine fracture zone: Journal of Geophysical Research, vol. 64, pp. 49-59.
Uchupi, E., J. D. Milliman, B. P. Luyendyk, C. O. Bowin, and K. O. Emery, 1971, Structure and origin of southeastern Bahamas: American Association of Petroleum Geologists Bulletin, vol. 55, pp. 687-704.




40 BUREAU OF GEOLOGY
Vail, P. R., R. M. Mitchum, Jr., R. G. Todd, J. M. Widmier, S. Thompson, III, J. B. Sangree, J. N. Bubb, and W. G. Hatlelid, 1977, Seismic stratigraphy and global changes of sea level: in Payton, Charles E. (editor), Seismic stratigraphy-Applications to hydrocarbon exploration: American Association of Petroleum Geologists Memoir 26, pp. 49-212.
Van der Voo, R., F. J. Mauk, and R. B. French, 1976, Permian-Triassic continental configurations and the origin of the Gulf of Mexico: Geology, vol. 4, pp. 177-180.
Walper, Jack L., and C. L. Rowett, 1972, Plate tectonics and the origin of the Caribbean and the Gulf of Mexico: Gulf Coast Association of Geological Societies Transactions, vol. 22, pp. 105-116.




INFORMATION CIRCULAR NO. 98 41
AUTHOR INDEX
Addington, J. W.........................37 Ibrahim, Abou-Bakr K................28
Anderson, Thomas H................19 King, Elizabeth R...................... 10
Andress, Noel E......................2, 9 Klitgord, Kim D....................10, 29
Applegate, Albert V.....................2 Krivoy, Harold L........................ 11
Applin, Esther R..........................3 Kriz, Jiri......................................14
Applin, Paul L......................... 2, 3 Ladd, John W............................30
Arden, Daniel D., Jr..................... 3 Latham, G...................................28
Ball, M. M..................................20 Loudon, E. J..............................34
Banks, J. E..................................4 Lynts, George W.......................30
Barnett, Richard S.......................4 Mauk, F. J................................. 33
Bass, Manuel N............................ 5 McMillen, K. J............................. 27
Beall, Robert.............................20 Milton, Charles..................... 11, 12
Behrendt, John C......................21 Mitchum, R. M., Jr.................... 33
Berdan, Jean M.................... 5,14 Mueller, Paul A..........................12
Bridge, Josiah.............................. 5 Mullins, Henry T........................30
Brown, Flett J............................. 13 Nafe, J. E..................................16
Bryan, G. M...............................14 Neathery, Thornton L................28
Buffler, Richard T................22, 28 Odom, A. Leroy.........................13
Campbell, R. B............................6 Osburn, William L.......................32
Carroll, Dorothy............................ 6 Palacas, James G.....................2...
Carye, J.....................................28 Paul, Charles K.........................25
Cavanaugh, T. D.......................27 Pilger, Rex H., Jr................13, 31
Chowns, T. M............................... 7 Pojeta, John, Jr.......................... 14
Cole, W. Storrs............................8 Popenoe, Peter.............10, 23, 29
Coney, Peter J.......................... 24 Porch, Jon W............................ 12
Cramer, Fritz H.................... 2, 8, 9 Pratt, Richard W..........................9
Crosby,. J. T................................ 14 Pyle, Thomas E.......................... 11
Daniels, David L........................23 Raschilla, S. N.......................... 34
Dickinson, William R................. 24 Reel, David A..............................9
Dietz, Robert S.................... 25, 27 Robb, James M.......................21
Dillon, William D ........... 25, 26, 29 Rowett, C. L.............................. 35
Drake, C. L......................... 16, 26 Schlee, John..............................21
Freeland, George L...................27 Schmidt, Victor A...................... 19
French, R. B.............................33 Schouten, Hans.........................10
Goldstein, Robert F................ 2, 9 Shaub, Jeanne F.......................22
Grasty, Robert.......................9,12 Sheridan, Robert E........14, 16, 32
Griffin, George M......................... 9 Silverstein, Katherine M............. 21
Hall, D. J................................... 27 Smith, Douglas M..........16, 17, 18
Harrison, C. G. A....................... 20 Sougy, Jean M. A...................26
Heirtzler, J................................. 26 Sproll, Walter P......................... 25
Henk, F. H., Jr........................... 34 Stoffa, P. L.......................... .... 14
Hennion, J................................. 16 Tanner, William F......................33
Hirshman, J.............................. 26 Todd, R. G.......................... .... 33
Holden, John C.........................25 Uchupi, Elazar............................28
Horton, J. Wright, Jr..................28 Van der Voo, R.........................33




42 BUREAU OF GEOLOGY
Waiper, Jack L.......17, 34, 35,36 Winston, George O ...................... 2
Watkins, Joel S...................22, 27 Wood, Michael L....................... 36
Wicker, Russell A......................18 Woods, R. D..............................37
Williams, C. T..............................7 Worzel, J. Lamar.......................22
Wilson, Gary V..........................19 Zeitz, Isadore...................... 23, 28
Wilson, J. Tuzo..................... 9, 36




INFORMATION CIRCULAR NO. 98 43
SUBJECT INDEX
Subject Author(s), Date Page
Florida Basement Geology:
age determ inations Andress, et al. 1969...................................... 2
Bass, 1969.........................................................5
Cam pbell, 1939................................................. 6
Cole, 1944.........................................................8
Cramer, 1973.....................................................8
Grasty and W ilson, 1967.................................. 9
M ilton, 1972..................................................... 11
M ilton and Grasty, 1969..................................12
Odom and Brown, 1972..................................13
Sm ith, 1982..................................................... 17
deep well data Applin, 1951..................................................... 2
Applin and Applin, 1965............................... 3
Barnett, 1975................................................... 4
Cam pbell, 1939................................................... 6
Cam pbell, 1940................................................. 6
Cole, 1944..........................................................8
Goldstein and Cramer, 1969.............................9
Grasty and W ilson, 1967.................................. 9
M ilton, 1972..................................................... 11
Milton and Grasty, 1969..................................12
geochem istry Carroll, 1963...................................................... 6
M ilton, 1972..................................................... 11
M ilton and Grasty, 1969..................................12
M ueller and Porch, 1983.................................12
geophysical data Arden, 1974.................................................. 3
Griffin, et al., 1977............................................ 9
King, 1959....................................................... 10
Krivoy, 1972.....................................................11
Sheridan, et al., 1981......................................14
Sheridan, et al., 1966......................................16
Sm ith, 1982..................................................... 17
W icker and Sm ith, 1978..................................18
W ilson, 1975....................................................19
heavy mineral
analysis Carroll, 1963...................................................... 6
paleogeography Applin, 1951..................................................... 2
Barnett, 1975................................................... 4




44 BUREAU OF GEOLOGY
Subject Author(s) Date Page
Bass, 1969.........................................................5
Cam pbell, 1940................................................. 6
Chowns and Williams, 1983.......................... 7
Cram er, 1971.....................................................8
Cram er, 1973.....................................................8
Klitgord, et al., 1984........................................ 10
Odom and Brown, 1976..................................13
Pilger, 1980..................................................... 13
Sheridan, et al., 1981......................................14
Sheridan, et al., 1966......................................16
Sm ith, 1983..................................................... 16
Sm ith, 1982..................................................... 17
W icker and Sm ith, 1978..................................18
paleontology Andress, et al. 1969...................................... 2
Cole, 1944......................................................... 8
Cram er, 1971.....................................................8
Cram er, 1973.....................................................8
Goldstein and Cramer, 1969.............................9
Pojeta, et al., 1976.......................................... 14
Sm ith, 1982..................................................... 17
petrography Bass, 1969.........................................................5
Carroll, 1963...................................................... 6
M ilton, 1972..................................................... 11
M ilton and Grasty, 1969..................................12
petroleum
potential Applegate, et al., 1981.................................. 2
Arden, 1974.................................................. 3
Banks, 1974.................................................. 4
review Barnett, 1975................................................... 4
Sm ith, 1982..................................................... 17
stratigraphy Applegate, et al., 1981.................................. 2
Applin and Applin, 1965................................ 3
Bridge and Berdan, 1951..................................5
Carroll, 1963...................................................... 6
Cole, 1944......................................................... 8
Goldstein and Cramer, 1969.............................9
Pojeta, et al., 1976.......................................... 14




INFORMATION CIRCULAR NO. 98 45
Subject Author(s) Date, Page
structure Applin and Applin, 1965............................... 3
Arden, 1974.................................................. 3
Banks, 1974.................................................. 4
Barnett, 1975................................................ 4
Bridge and Berdan, 1951............................. 5
Chowns and Williams, 1983............................. 7
King, 1959....................................................... 10
Klitgord, et al., 1984........................................10
Krivoy, 1972....................................................11
Sheridan, et al., 1981......................................14
Sheridan, et al., 1966......................................16
Sm ith, 1983..................................................... 16
Sm ith, 1982..................................................... 17
W icker and Sm ith, 1977..................................18
W ilson, 1975....................................................19
tectonics Barnett, 1975................................................... 4
Chowns and Williams, 1983............................. 7
Cram er, 1971.....................................................8
G rasty and W ilson, 1967............................... 9
King, 1959....................................................... 10
Klitgord, et al., 1984........................................ 10
Krivoy, 1972.....................................................11
Odom and Brown, 1976.................................. 13
Pilger, 1980..................................................... 13
M ueller and Porch, 1983.................................12
Sheridan, et al., 1981......................................14
Sheridan, et al., 1966......................................16
Sm ith, 1983..................................................... 16
Sm ith, 1982..................................................... 17
W alper, 1974................................................... 17
Related Regional and Tectonic Studies:
Baham a platform Dietz, et al., 1970............................................25
Freeland and Dietz, 1971............................... 27
Mullins and Lynts, 1977.................... ............... 30
Sheridan and Osburn, 1975............................32
breakup of
pangaea Anderson and Schmidt, 1983......................... 19
Ball and Harrison, 1969.................................. 20
Dietz, et al., 1970............................................25
Freeland and Dietz, 1971............................... 27
Klitgord, et al., 1983........................................29




46 BUREAU OF GEOLOGY
Subject Author(s) Date, Page
Ladd, 1976.......................................................30
Mullins and Lynts, 1977..................................30
Pilger, 1978................................. ................. 31
Walper, 1980................................................... 34
Walper, et al., 1979.........................................35
Walper and Rowett, 1972............................... 35
Wilson, 1966....................................................36
Wood and Walper, 1974.................................36
Woods and Addington, 1973.......................... 37
Caribbean Anderson and Schmidt, 1983......................... 19
Ball and Harrison, 1969.................................. 20
Freeland and Dietz, 1971............................... 27
Ladd, 1976.......................................................30
geophysical data Behrendt, et al., 1974..................................... 21
Buffer, et al. 1980...........................................22
Daniels, et al., 1983........................................ 23
Dillon and Paul, 1982......................................25
Drake, et al., 1963.......................................... 26
Hall, et al., 1982..............................................27
Horton, et al. 1984.......................................... 28
Ibrahim, et al., 1981........................................28
Ibrahim, et al., 1982........................................28
Klitgord, et al., 1983........................................29
Ladd, 1976.......................................................30
Sheridan and Osburn, 1975............................32
Todd and Mitchum, 1975................................ 33
Gulf Coast basin Beall, 1973.......................................................20
Wood and Walper, 1974.................................36
Woods and Addington, 1973.......................... 37
Gulf of Mexico Anderson and Schmidt, 1983......................... 19
Ball and Harrison, 1969.................................. 20
Beall, 1973.......................................................20
Buffler, et al., 1980..........................................22
Dickinson and Coney, 1980............................24
Hall, et al., 1982..............................................27
Ibrahim, et al. 1981......................................... 28
Ibrahim, et al., 1982........................................ 28
Pilger, 1978..................................................... 31
Tanner, 1965................................................... 33
Todd and Mitchum, 1975................................33




INFORMATION CIRCULAR NO. 98 47
Subject Author(s) Date Page
Van der Voo, 1976..........................................33
Walper, 1980...................................................34
Walper, et al., 1979.........................................35
Walper and Rowett, 1972............................... 35
Wood and Walper, 1974.................................36
opening of the
North Atlantic
Ocean Behrendt, et al., 1974..................................... 21
Dickinson and Coney, 1980............................24
Dietz, et al., 1970............................................ 25
Ladd, 1976.......................................................30
Pilger, 1978...................................................... 31
Wilson, 1966....................................................36
petroleum
potential Dillon and Paul, 1982......................................25
Sheridanvand Osburn, 1975.............................32
Woods and Addington, 1973.......................... 37
pre-Atlantic
Ocean
reconstruction Anderson and Schmidt, 1983......................... 19
Behrendt, et al., 1974..................................... 21
Dickinson and Coney, 1980............................24
Dietz, et al., 1970............................................25
Freeland and Dietz, 1971............................... 27
Klitgord, et al., 1983........................................29
Mullins and Lynts, 1977..................................30
Pilger, 1978.....................................................31
Van der Voo, et al., 1976............................... 33
Walper, 1980................................................... 34
Walper and Rowett, 1972............................... 35
Wilson, 1966....................................................36
southeastern United
States Coastal
Plain Daniels, et al., 1983........ .................................. 23
Horton, et al., 1984........................................ 28
Klitgord, et al., 1983........................................29
stratigraphy Dillon and Paul, 1982.......................................25
Todd and Mitchum, 1975................................33
structure Behrendt, et al., 1974............................... .... 21
Daniels, et al., 1983......................................... 23




48 BUREAU OF GEOLOGY
Subject Author(s), Date Page
Dillon and Paul, 1982......................................25
Drake, et al., 1963.......................................... 26
Horton, et al., 1984................................... .... 28
Ibrahim, et al., 1981........................................ 28
Klitgord, et al., 1983........................................29
West Africa Behrendt, et al., 1974..................................... 21
Dillon and Sougy, 1983...................................26
Todd and Mitchum, 1975................................33




INFORMATION CIRCULAR NO. 98 49
APPENDIX
FLORIDA DEEP WELL DATA
Well location maps are available from the Florida Geological Survey.




FLORIDA DEEP WELL DATA
(Primarly wells which penetrated basement, but including oomv bignifloant wells which did not)
Depth to and
Well and Completion Eiev. of Total Depth Type of Bsaement Penetration
County Permit No. Well Name Locatlon Date Well8, ft. of Well, ft. Reference Rook Encountered of Basement, ft. Comments
Ala chus W.1465 Tidowater Aseoc. Sea. 23 1947 112 3150 Applin, 1951 quartltic sandstone 3135/15
P.49 Oil Co.-R.H. TOA RISE & shale, Paleozolo Cato No. 1
W.1472 Tidewater Assoc. 8e. 24 1947 132 3220 Applin, 1951 quartaltic sandstone 3217/11
P.52 011 Co.-J.A. TO8 R21E & shale, Paleosolo Phifer No. 1
W-1487 Tidewater Assec. Se0. 33 1947 168 3220 ApplIn, 1951 quafltltlc sandstone 3170/50
P.54 Oil Co.--Jodle 1T78 R1OE & shale, Patloozolo Parker No. 1
W.11447 Chevron.Container Sea. 7
P.536 Corp. 1 TBS R21E 1972 168 2861 Barnett, 1978 Ordovlolan quartzite; 2606/255 no voloanlsce
W.12226 Chevron. Sea. 34 1974 150 3340 Bamrnett, 1975 Ordovician quartzite; 3314/26
P-700 Donaldson I TOS R21E no voicanice
Baker W.1500 Hunt OIl Co.. Sec. 21 1947 130 3349 Applln, 1951 Paleozolo quartzltlo 3342/7
P-59 H. L. Hunt No, 1 T1N R20E sandstone
Bay W.12498 Charter Expl. 2- Sea. 27 1973 67 12313 Barnett, 1975 granite 12256/55
P-690 St, Joe Paper Co. TIS R17W
W.14844 Houston 011 & Seac. 13 1980 105 12486 No published
P-1010 Mlnerals-SW T28 R12W Information.
Forest Industries
133 No. 1
Bradford W-1466 Tidewater Assoo. Se.15 1947 141 3167 Appiln, 1951 Quartaltic sandstone 3140/27
P-41 Oil Co.-M,F. TOS R20E & shale, Paleozolo Wiggins No. 1
W-10798 Inexoo Ol Co. Sec. 22 1970 148 3154 Bamrnett, 1975 Paleozolo quartztlc 2984/170
P-405 Gilman Paper T458 R22E sandstone
Calhoun W-12812 Mallard Explora- Sea. 31 1975 111 12140 No published
P-777 tlon Inc.. T1S R10W Information.
International
Paper Co. 31-2
1. Florida Bureau of Geology well number.
2. Unless otherwise Indicated, these are drill floor elevations (In feet above MSL).




FLORIDA DEEP WELL DATA
(Primarily wells which penetrated basement, but Including some significant wells which did not)
Depth to and
Well1 and Completion Elev. of Total Depth Type of Basement Penetration
County Permit No. Well Name Location Date Well2, ft. of Well, ft. Reference Rock Encountered of Basement, ft. Comments
Charlotte W-979 Humble Oil & Re- Seo. 17 1945 20 13304 Applin, 1951 Did not reach
P-5B fining Co.- T428 R23E basement; TD In Lowndes-Treadwell Lower Cretaceous. No, IA
W-8139 Mobile Oil 1 82320'28"W 1967 64 12931 Bamrnett, 1975 pseudospherulltlc 12877/54 170 + 4 my (Mobil).
P-375 State Lease 224B 42,424' from granophyre USGS Englowood
W-10717 Exchange O&G 1- Sec. 7 1970 80 13432 Bamett, 1975 DId not reach I P-459 Payson T418 R27E basement; TD In upper 0 part basal clastic
section, L Cret.
Citrus W-7534 Mobil Oil 1 Sec. 12 1965 115 4490 Barnett, 1975 Paleozolo quartzitlc 4430/60
P-358 Camp Phosphate T178 R1SE sandstone; no voicanics O
W-7538 Mobil Oil 1- Sec. 25 1965 24 4794 Bamrnett, 1975 Paleozoic quartzitic 4738/56 Z P-353 Harbond T178 RISE sandstone; no volcanicel O
W-7543 Mobil Oil 1 Sec. 8 1965 13 5556 Bamrnett, 1975 Paleozolo quartzitic 5520/36
P-350 Garby T198 R17E sandstone; no volcanics
C
W-8304 Mobil Oil Al 2850'00"N 1967 11 6041 Bamrnett, 1975 quartzitic sandstone 5886/34 Devonlan (Mobil
P-382 State Lease 224A 82'49'42"W paleo).'
Clay W-1590 Humble Oil & Re. Sec. 4 1947 115 5862 Applln, 1951 Paleozolo quartzltic 3725/2137 z
P-50 fining Co, Fore- TS R25E sandstone most Properties Corp. No. 1 (
Collier W-961 Humble Oil & Re. Seo. 30 1944 34 13512 Applln, 1951 Did not reach baseNo permit fining Co. Gulf T48S R30E ment; TD In Lower Coast Realities Cretaceous. Corp. No. 2
W-12838 Bass Enterprises Sec. 12 1975 (KB)30 18670 Applegate, et Igneous rock 18610/60
P-778 Prod. Co. Collier T52S R27E al., 1981 Co. 12-2
W-15122 Exxon, Collier Co. Sec. 20 1981 45 17200 No published InforP-1042 Well No. 20-2 T48S R30E mation.1. Florida Bureau of Geology well number.
2. Unless otherwise Indlicated, these are drill floor elevations (In feet above MSL),




FIOHI[)A DEt WEIL DA FA
(Primlarily walle wlwih pentratwd babirernit, but includinrUg iomre blUnflrUinlt well1 which did nol)
Depth to and
Well' and Completion Elev, of Total Depth Type of Baswerent Penetration
County Permit No. Well Name Location Date Well1, ft. of Well, it. Reference Rock Encountered of Basement, ft. Comments
Columbia W.1789 Humble Oil & Re. Sea. 22 1948 141 4444 Applin, 1951 Weathered sone; 3482/10
P.77 fining Co. J.P. T1N R17E
Cone No. 1 Paleozolo black shale; 3492/952
diabase and amygdular 3529/33
basalt silla encountered 3584/1 Not studied petrographically. In the black shale 4191/1 Not studied petrographically, 4193/2
4248/3
4267/3
W-1832 Sun Oil Co. Sec. 24 1948 138 3311 Applin, 1951 Paleozolo black shale 3303/68
P-93 M. W. Sapp No. 1A T28 RIE
W-1915A Sun Oil Co. Sec. 27 1949 87 3051 Applin, 1951 Paleozolo quartzltlo 3033/18
P.104 W. F. Johnson No. T4S RIE sandstone
1
W.1923 Sun Oil Co. Sec, 11 1949 124 2929 Applln, 1951 quartzltlc sandstone 2922/7
P.107 Clarence Loyd No. TSS R17E & shale, Paleozolo "
1 0
W-1981 Sun Oil Co. Sec. 10 1949 174 2828 Applln, 1951 quartzltlc sandstone 2813/15
P-111 Ruth M. Bishop T48 R17E & shale, Paleozolo No. 1
W-2164 Guff Ot Corp. Sec. 2 1950 117 3470 Bridge & Late Silludan or not given Age esUtimate based
P.124 Ke Vining No, 1 T4S R15E Berdan, 1951 Early Devonian on fossiell and Ithoblack shale logic correlations
Goldstein, et Late Silurian or 3350/? Siluran(?) chitinozoans al., 1969 Early Devonlan recovered from sample: black shale 3350-3450 ft.
W.8585 Richard C. Bradley Sec. 25 1968 80 3115 Barnett, 1975 Paleozolo quartzltlc 3104/11
P.399 1 J. M. Carter T5 RISE sandstone, no volcanice
W.8586 Richard C, Bradley See. 16 1968 96 3097 Barnett, 1975 Paleozolo quartzitlo 3084/13
P-390 1 Brunswick Pulp TOS R17E sandstone, no volcanlce & Paper
W.11830 Getty Oil Co. 1 Sec. 21 1973 191 2898 Barnett, 1975 Paleozolo (Getty) 2848/42 Bamett did not
P-653 Holmes 21-8 T38 R17E examine.
1 F!. -- .. o. .ec!gy woll number.
. Intsaa ntharwla Indicated, theme are drill floor elevati on fin fet above M1SL.




FLORIDA DEEP WELL DATA
(Pdrimarily wells which penetrated basement, but Including some signifloant wells which did not)
Depth to and
Well and Completion Elev. of Total Depth Type of Basement Penetration
County Permit No. Well Name Location Date Well2, ft. of Well, ft. Reference Rock Encountered of Basement, ft. Comments
W-11910 Getty Oil Co. 1 Sec 33 1973 157 3196 Barnett, 1975 Paleozoclo (Getty) 3125/71 Bamett did not
P-666 J. C. Marsh T28 R17E examine.
W-14379 Shepherd 011 & Sec. 8 1979 194 3013 No published InforP-986 Gas, Inc. T4S RISE mation.
Shepherd-Rayonler
No, 1
Dade W-889 Humble Oil & Re- Sec. 30 1945 15 11794 Applln, 1951 Did not reach baseNo permit fining Co. State TOSS R36E ment; TD In Lower of Florida No. 1 Oretaceous. 0
DeSoto W-11766 Shell OIl 1 Sec. 22 1972 (KB)77 1300 Barnett, 1975 Did not reach baseP-609 Shell Punta Gorda T39S R27E ment; TD In basal plastic section,
Lower Cretaceous. 0
z
W-12393 Amoco Prod. 1 Sec. 19 1974 119 11655 Barnett, 1975 Jurassic diabase, 11627/28
P- 679,
679A Opal Knight T3S R27E resembling Polk &
Hardee County wells
Dixie W-1 114 Stanollnd Oil & Sect. 5 1946 33 7510 Applln, 1951 Paleozolo quartzltic 5228/2282
P-11 Gas Co. & Sun Oil T118 R11E sandstone Co.,- Perpetual
Forest, Inc. No. 1 Z
W-1405 Sun Oil Co. Sec. 8 1946 33 3671 Applln, 1951 quartzltl sandstone & 3645/26 0
P-38 Hazel Langeton TOS R14E shale, Paleozolo
No. 1 C
W-1863 Sun Oil Co. Sec. 36 1949 41 5104 Applln, 1951 Paleozolo sandstone & 5016/68
P-97 P. C. Crappe "A" TS R10E shale Well No. 1
1. Florida Bureau of Geology well number.
2. Unless otherwise Indloated, these are drill floor elevations (in feet above MSL).




FLORIDA DEEP WELL DATA
(Primarily wells which penetrated basement. but Inckluding some signifcanl wels which did not)
Depth to ad
Wel1 and Completion Elev of Total Depth Type of Basement Penetraton
County Permit No. Wel Name Location Dale Wel01, ft. of Well, ft. Reference Rock Encountered of Basement, ft. Comments
Duval W-4881 T. A. Durham 1 Sec ,23 1960 81 4192 Bamrnett, 1975 Paleozoi; no volcanlcs 4151/41 Penetration using P.402 Monticello Drug T18 R25E (logger) ogers TD.
4250 4151/90 Penetraton using (Barmett) Banett's TD.
WSOMO T. A. Durham B1 -Sec. 17 1969 94 3521 Barnett, 1975 Pleozoic quatltIc 3458/03
P-410 Gilman Paper T38 R23E sandstone; no voloanien
W.10302 T. A. Durhamn 1 Sc. 11 19609 95 3743 Barnett, 1975 Palsozol quante 3637/1060
P.404 Ollman Paper T38 R235 sandstone; no volcanlcs
Escembla W.15013 Chevron USA Inc. -Sec. 2 1981 256 17950 No published Infor.
P.1027 La Floreta Well T3N FR33W maion.
No. 2-1
Flagler W.1473 Humble Oil & Re. So. 8 1947 31 4632 Applln, 1951 tuff & volcanic 4588/44 Mixed tuff derived
P-44 fining Co. J. W. 7118 R28E agglomerate of rhyolllc from Igneous complex.
Campbell No. 1 compoaltion Origion sedimentary or explosive Igneous.
Base, 1969 tuff, richer In CaO (Bass examined Mineral comp. Indlthan rhyolte core from this catese Incomplete
lower Interval; adJ. to conditions
exact depth un- of greenechist
known due to faces.
mislabeing.)
Frankliln W-4487 Mobil Prod. C10 N42'03'47"E 1973 37 (Bamett) 14824 Barnet, 1975 Eagle Mills Fm. 138650/434 Penetration using
P.387 State Lease 224A 121,639.31' from (Subsequenty original TD of 14,284.
Tri-Statilon St. drilled to First dlabase sll 1392637 No Informatllon George blghthouse 14369) publIshed on subsequent drilling.
Glichrist W-1003 Sun Oil Co. Sec. 15 1946 93 3753 ApplIn, 1951 qualtic sandstone 358/165
P-5 Alto Adamre No. 1 T9S R1SE & shale, Paleozolc
W.1819 Sun Oil Co. Sec. 12 1948 77 3348 Applin, 1951 quarultic sandstone 3348/18
P.-89 Williams Bros. TSS R15E & shale, Paleozolc No. 1
1. Florida Bureau of Geology well number.
:. ...... .., :. "-..Z are dr:U f ocr :vations (In feet above MSL).




FLORIDA DEEP WELL DATA
(Primarily wells which penetrated basement, but Including some significant wells which did not)
Depth to and
Well1 and Completion Elev. of Total Depth Type of Basement Penetration
County Permit No. Well Name Location Date W1el2, ft. of Well, ft. Reference Rock Encountered of Basement, ft. Comments
Gulf W-12483 Charter Expl. & Sec. 26 1973 34 14297 Barnett, 1975 daclt porphyry (ash 14261/36 core: 14261-14297
P-e70 Prod. 1 St. Joe T8S RO10W fall tuff, red brown, oblique fractures: Paper Co. massive appearance) 14264 & 14267.
W-12509 Hunt OIl 30-4 Sec. 30 1974 81 13284 Barnett, 1975 granodlorite, Late 12898/386
P-748 International T3S R11W Precambrian or Early
Paper Cambrian?
Krueger Enter- 12,950-12,990:709 25my, prices, 19813 K-Ar age determined from feldspar concentrate
W-12617 Charter Expl. Sec. 12 1975 22 14574 Barnett, 1975 Upper Paleozoio or 14499/75 Coarse quart tic as
P-762 Prod. 6 St Joe TSS RO10W Lower Trassic with Ithic & feldsPaper Co. pathic fragments, orange claystone &
red shale. Weathered
zone at top.
W-14173 Mesa Petroleum- Sec. 29 1980 47 14186 No published
P.957 St Joe Paper Co. T5S R9W Information.
29-4 Well No. 1
Hardee W-1655 Humble 011 & Re- Sec. 23 1948 83 11934 Applln, 1951 Lava & pyroclastic 11828/106
P-62 fining Co. T35S R23E rocks P
B. T. Keen No. 1 Bass, 1969 basaIlt (Bass ex- Least altered of amined core volcanic rocks
from 11930- studied from
11932) Florida.
Milton & 11,853; whole rock K-Ar Grasty, 1969 age determinations: 143 t 7 my, 147 t 3 my
1. FlorIda Bureau of Geology well number.
2. Unless otherwise Indicated, these are drill floor elevations (In feet above MSL).
3. Unpublished age determination (memo on file at Fla. Bureau of Geology); material submitted by H. Kelley Brooks to Krueger Enterprises, Inc., Geochron Laboratories Division.




FLORIDA DEEP WELL DATA
(Primarily wells which penetrated basement, but includin0 somo significant walls which did not)
Depth to and
Well and Completion Elev. of Total Depth Type of Basement Penetration
County Permit No. Well Name Location Date Well, Ft. of Well, ft. Reference Rock Encountered of Basement, Ft. Comments
Hendry W-11504 PhIllips 10 Soc. 26 1972 (KB)36 17028 Barnett, 1975 tuffaceous detritus TD In bal clastic
P-565B Seminole Tribe T468 R33E (? see comments) seollont Low Cre.
top 16812 (Phillips).
Exxon ret
tuffeeous detitus
in last samples.
W-126906 Shell Oil Company Sec. 19 1975 44 16000 Applegate, St Did not penetrate P.768 1 Alloo Land & T458 R32E al., 1981 basement, TD in
Dev. Wood River Fm., probably Late
Jurassic.
Hernando W.994 Ohio OIl Co. 8ec. 19 1946 47 8472 Applln, 1951 Paleozolo quartUzltic 7720/752
P.1 Hemasco Corp. T238 RISE sandsatones
No. 1 0 11
W.8188 8. Davis & G. Soc. 32 1968 82 6209 Barnett, 1975 quattltc sand. 6190/19
P-378 Thayer 2 Hill T228 R21E stone; no volcarlice
W.8533 S. Davis & G. Sec. 11 1968 151 6764 Barnett, 1975 quartitl sand- 8640/124
P-391 Thayer 1 Davis T238 R20E stone; no voicanics
Highlands W-966 Humble OIl & Re- Soc. 34 1946 114 12985 Applin, 1951 Amygdaloldal basalt, 12618,367
P-B-1 fining Co. C.C. T388 R29E rhyolite porphyry and Carlton Estate No. related volcanic rocks
1 Milton & 12,664; whole rock K-Ar Grasty, 1969 age determination: 183 t 10 my
W-3578 Continental Oil Sec. 20 1955 88 12630 Applin & Pr-Mesozoic 12602/28
P-225 Co. C. C. Carl- T38S R28E Applin, 1965 volcanic rocks ton et al. Well No. 1
W-13502 Amoco Prod. Co. Seo. 6 1977 25 12625 No publIshed Infor.
P-862 No. 1 Andrew T39 RF30E motion.
B. Jackson 6-2
1. Florida Bureau of Geology well number.
2. Unless otherwise Indicated, these are drill floor elevations (In feet above MSL).




FLORIDA DEEP WELL DATA
(Primarily wells which penetrated basement, but Including some significant wells which did not)
Depth to And
Well1 and Completion Elev. of Total Depth Type of Basement Penetraion
County Permit No. Well Name Location Date Wel2, ft. of Well, ft. Reference Rock Encountered of Basement, ft. Comments
Hillsborough W-1005 Humble Oil & Re- Sec. 7 1946 112 10129 Applin, 1951 rhyolite & volcanic 10,010/119
P.29 fining Co.- T. S. T316 R22E agglomerate Jameson No. 1
Bass, 1969 Intermediate to basic (Bass examined Incomplete adj. to composition core from conditions of 10,106-10,115) greenschst faces. j
Holmes W-12199 Sonat Expi-Randall Sec. 32 1974 140 11201 Bamrnett, 1975 Eagle Mills fm. 10240/61 0
P-716 Hughs T4N R17W red arkosic sands & granite wash.
Diabase, greenish 10940
& weathered top
0
Indian River W-3763 Amerada PetroleumSec. 28 1956 60 9488 Applin & Pre-Mesozoic 9410/78 Z
P.243 Corp. Fondren T318 R35E Applin, 1985 volcanic rocks.
Mitchell Well No. 1
0
Jackson W-1888 Humble Oil Re- Sec. 8 1949 128 9245 Applin, 1951 Paleozoic red & gray 8440/805 C
P-94 fining Co. TSN R11W sandstone & shale.
C. W. Tindel No.
Two (Triasucl?) basalt 8890/42 Porphyritic homblende z sills in Paleozolo basalt Intruslve O strata. or flow.
8970/13 Not studied petrographically. *
Jefferson W.1854 Coastal Petroleum Sec. 1 1949 51 7913 Appiln, 1951 Triassic (?) disbase 7763/29
P-95 Co. E. P. Larsh T2S R13E & related Igneous rocks. 7850/40 No. 1 (Sills or dikes In plastic rocks of Triassic (?) age.)
Paleozoic (?) quartzitlc 7909/4
sandstone.
1. Florida Bureau of Geology well number. 0,
2. Unless otherwise Indicated, these are drill floor elevations (In feet above MSL).




FLORIDA DEEP WELL DATA i (Primarily wells which penetrated basement, but Including some significant wells which did not) l
Depth to and
Well1 and Completion Eiev, of Total Depth Type of Basement Penetratlon
County Permit No. Well Name Location Date Well8, ft. of Well, ft. Reference Rock Encountered of Basement, ft. Comments
W*10015 Amooo Prod. 1 Seo. 17 1971 65 7034 Barneltt, 1975 Eagle Mille finm. 6600/160
P-400 Buckeye T26 R5
Paleosoilo sandstone. 6748/280
Diabase. 606/6
Gabbrolo diabase. 8730/13
Gabbrolo dlabase. 8793/131 C
Lafayette W*968 Sun Oil Co. e80, 25 1946 70 4133 Applln, 1951 quartUltic sandstone & 4030/103
P.4 P. C. Crappe No, 1 TOS R12E shale, Paleozoo.
W-18908 Humble Oil & Re. Soc. 20 1948 62 4235 Applin, 1951 quartzftlo sandstone & 4205/30
P-67 fining Co.- T4S R11E shale, Paleozolo R. L. Henderson No. '
1 0
W*1860 Coastal Petroleum Sec.18 1949 46 3507 Applln, 1951 quatzlto sandstone & 3480/27 O
P-100 Co. Ronald SappT8S R14E shale, Paleozolo No. 1
W.2000 Gulf Oil Corp. Se. 36 1949 87 4505 Applln, 1951 Paleozolc quartzltlc 4505/7
P-114 Brooke Scanlon 7T5S R10E sandstone.
Inc., Block 40,
Well No. 1
No. W-no. Hunt Oi 1A P.C.See. 21 1974 74 5501 Barnett, 1975 Paleozolo shade & sand. 3716/1785 No samples available.
P-725A Crappe 768 R13E stone, no voloanlce
W-15078 Amoco Prod. Co. -Sec. 33 1981 82 10078 No published InforP-1052 P. C. Crappe No. 1 T6S RIlE motion.
1. Florida Bureau of Geology well number.
2. Unless otherwise Indicated, these are drill floor elevations (In feet above MSL.)




FLORIDA DEEP WELL DATA
(Primarily wells which penetrated basement, but Including some significant wells which did not)
Depth to and
Well1 and Completion Elev. of Total Depth Type of Basement Penetration
County Permit No. Well Name Location Date Well2, ft. of Well, ft. Reference Rock Encountered of Basement, ft. Comments
Lake W-275 Oil Development Sec. 17 1937 120 6120 Applin, 1951 granite 6103/17 No permit Co. of Fla. J. T24S R25E
Ray Arnold No. 1
W-11499 Hamilton Bros. 1 -Sec. 25 1972 92 5397 Bamrnett, 1975 weathered basic Igneous 6195/202
P-574 Keen T208 R26E rock
W.11771 Amoco Prod. 1 Sec. 5 1972 127 5778 Bamrnett, 1975 slaskite 5690/10 P-629 Arnold Ind. T24S R25E weathered Igneous 5747/31
W-12891 Amoco Prod. 1 Sec. 29 1975 (KB)56 4894 No published InforP-795 USA 29-13 T16 R28E motion.
0
Lee W-10566 Humble 1 LehlghSec. 14 1970 57 15710 Bamrnett, 1975 altered quartz diabase 15675/35 163 m.y. (Exxon) Z P-407 Acres T458 R27E
Leon W.12293 Phillips Petr. Seo. 14 1974 33 10466 Barnett, 1975 Eagle Mills fm, 8450/2016
P-717 1 St. Joe A T28 R1E Dlabase sills 8488/88 0 9208/46 C 9316/5
9356/10
O9380/2
9394/8
948/29Z
10239/33 O 40
Levy W-1007 Sun Oil Co. Sec. 31 1946 34 3997 Applin, 1951 Paleozolc quartzltic 3960/37 C
P-13 J. T. Goethe T148 R17E sandstone No. 1
W-1537 Coastal Petroleum Sec. 16 1947 14 5850 Applin, 1951 Paleozolo black shale 5810/40
P-6 Co. J. B. & J. T. TISS R13E
Ragland No. 1
1. Florida Bureau of Geology well number.
2. Unless otherwise Indicated, these are drill floor elevations (In feet above MSL.)




FLORIDA DEEP WELL DATA
(Pimarily wells which penetrated basemennt, but including borne slgrnilficanlt wells which did nol)
Depth to and
WefoI' and Completion Elev. of Total Depth Type of basement Penetration
County Permit No, Well Name Location Date Will8, ft. of Well, ft. Reference Rock Encountered of Basement, ft. Comments
W-2012 Humble Oil & Re- Sec. 19 1949 s 400 Applin, 1951 Decomposed Igneous rock4317/27 underlies L. Cret. so.
P.105 fining Co. C. E. T158 R17E
Robinson No, 7 Triassc? basalt 4344/33
Paleosolo-altered black 4377/0.5
shale
Paleoolc quartzltlc 4377.5/231.5
sandatone
W-8305 Mobil Oil 1B 838'41'36 1967 24 4735 Barnett, 1975 quartitic sandstone, 4595/140 Devonian (Mobile
P-383 State Lease 224A 45,733 ft very fine grained, well paleo) from USGS sorted, tight "Lukens"
Uberty W.12496 Placid Oil 26-4 Sec. 26 1974 62 12131 Barnett, 1975 Eagle MIls fm. 11753/378
P.730 USA T38 RSW
Diabase ells 12060/10
12095/36
W.12497 Placid Oil 16-3 Sec. 16 1974 74 12400 Bamrnett, 1975 Altered granophyre 12040/360
P-745 USA T48 R6W
W-12739 Placid Oil 10-3 Sec. 10 1975 75 12654 Barnett, 1975; TD In Louann
P-769 USA T48 R7W Applegate, et (Juraslo).
al., 1981
Madilson W-15906 Hunt OIl Co. Sec. 6 1944 107 5385 Appiln, 1951 Triassic? dlabase 4589/39 Underles L Cret.
No permit J. W. GIbson No. 2 T1S R10E or older Mesozlo rock.
Paleozolc black shale 4628/757
W-1598 Hunt Oil Co. Sec. 5 1945 73 4096 Applin, 1951 Triasic? diabase 4044/16 Underles L Cret.
No permit J. W. Gibson No. 4 T28 R11E or older Mesozolo rock.
quarzltlc sandstone & 4060/36
shale, Paleozolo
W-15017 Amoco Prod. Co. Sec. 22 1981 114 10149 No published Infor.
P-1033 No. 1 Gilman T28 R9E rnmallon.
Paper Co.22-2
1. Florida Bureau of Geology well number.
2. Unless otherwise Indicated, these are drill floor elevations (In feet aove MSL).




FLORIDA DEEP WELL DATA
(Primarily wells which penetrated basement, but including some significant wells which did not)
Depth to and
Well' and Completion Elev. of Total Depth Type of Basement Penetration
County Permit No. Well Name Location Date Well2, ft. of Well, ft. Reference Rock Encountered of Basement, ft. Comments
Manatee W.12691 Amoco Prod. 1 -I Sec. 35 1975 130 11500 Barnett, 1975 TD In basal clastic
P-759 St. Petersburg T338 R20E section, L CreMt.
Maron W-18 Ocala OII Corp. Sec. 10 1928 80 6180 Applin & mica schist & quartzite, 4100/2080 Campbell, 1939, assigned
No permit No. 1 York T168 R2OE Applin, 1944 age uncertain Jurassic age.
(Applin, 1951 refers
to this well as Paleozoic quartzltlc 4100?/2080? Cooke, 1946, gave a Ocala Oil Corp. sandstone probable Paleozolo Clark-Ray Johnson age. No. 1)
W.901 J. 8. Cobden Sec. 25 1928 195 4334 Applin, 1951 Paleozolc quartzltlc 3860?/6747
No permit W. L Lawson No. 1 T188 R20E sandstone
1. FlorIda Bureau of Geology well number.
2. Unless otherwise Indicated, these are drill floor elevations (in feet above MSL.)
C
a




FLORIDA DelP WELL DATA 8 (Primedly weli wth penetrated bement, but including ome significant wells which did not)
Depth to and
WellON' and Completion Elev, of Total Depth Type of Basement Penertration
County Permit No. Well Name Location Date Well, ft. of Well, It. Relerenoe Rock Encountered of Saeentb, ft. Comments
Maron, (cont,) W*1482 Sun Oil Co. Sec. 15 1947 74 4037 Applin, 1901 Paleozolo (Lower 4240/376 P-3 Henry N. Camp TI18 R23E Ordoviolan) quartatic No.1 sandstone
Volcanic agglomerate or 4015/22 derived from an tuff a hyolt lo compo. Igneous complex action
Bass, 1960 queatzito sandstone 4240450 PaoIble Crelsaeous age for tthe quart.
atlo se & the
arhosio conigi. &
N should not be
oxluded In favor
of Pasozol. 0 volcanic aggolmerate or 4615/22 Arkoelo roofks are tuft lIthologiesly different from those of equiv. age
elsewhere In 1i.;O therefore, a nearby fault sorp Is
postulainod, alon
with a crystaline
source eas of the welt.
W-1904 Sun Oil Co. Sec. 24 1949 79 3845 Applin, 1951 Paleozolo quartzitlc 3679/166
P-101 H. T. Parker No. T148 R22E sandstone
1
Krueger Enter- 3845': 424 : 15 my, prises, 1981 K-Ar age determined from muscovite concentrale.
1. Florida Bureau of Geology well number.
2. Unless otherwle Indicated, these are drill floor elevations (In feet above MSL).
3. Unpublished age determination (memo on file at Flae. Bureau of Geology); material submitted by H. Kelley Brooks to Krueger Enterprises, Inc,, Geochron Laboratories Divilon.




FLORIDA DEEP WELL DATA
(Primarily wells which penetrated basement, but Including some significant wells which did not)
Depth to and
Well and Completion Elev. of Total Depth Type of Basement Penetmration
County Permit No. Well Name Location Date Well2, ft. of Well, ft. Reference Rock Encountered of Basement, ft. Comments
Martin W-14960 Kanaba Oii Sec. 21 1981 44 13198 No published inforP-1032 Corp. Allapattah T38S R39E motion.
Properties 21-1
Monroe W-445 Peninsular Oil & Sec. 6 1939 14 10006 Applin, 1951 Did not reach baseNo permit Refining Co. TS8 R34E ment; TD In Lower J. W. Cory No. 1 Cret.
W-972 Gulf Oil Corp. See. 2 1947 23 15455 Applin, 1951 Did not reach base-.
P-22 State of Fla. T67S R29E ment; TD In Lease No. 373 Jurassic(?).
Nassau W-33 St. Mary's River Soc. 19 1940 110 4824 Appln & Palozoic black shale 4640/168 The black shale has
No permit Oil Corp. T4N R24E Applln, 1944; been variously Hilliard Turpen- Applin, 1951 Triassic: Diabase sill 4808/16 assigned Mississipplan, tne Co. No. 1 or dike Pennsylvania, Triasslo & Jurassic agsa age
Cole, 1944 Triassic black shale 4840/155 still appears to be Igneous rock 4795/29 uncertain.
Triasslo? diabase sill 4808/16
or dike.
W-10715 Amoco Prod. 2-1-TT' Sec. 50 1970 34 5489 Barnett, 1975 Paleozolo quartztic 5086/3730
P-449 Rayonler T3N R27E sandstone
Triassic diabase sills 5260/15
5310/15
5418/51
Okaloosa W-11487 Sonat Expl. 1 Sea. 3 1972 170 14514 Barnett, 1975 Eagle Mills fm 14095/419 14100-14480: quartaltc
P-590 J. G, Moore 3-11 T3N R24W sandstone; 14480-14514: Diabase (log Sonat) 14478 contact welded quartzite
& v. coarse diabase.
1. Florida Bureau of Geology well number.
2. Unless otherwise Indicated, these are drill floor elevations (in feet above MSL).




FLORIDA DEEP WELL DATA
(Primarnenly well which penertrated basement, tout Including some sigrficfnt wells which did not)
Depth to end
Well' end Lomple tion Elev. of Total Depth Type of Basement Penetration
County Permit No, Well Name Location Date Well8, ft. of Well, ft. Reference Rock Encountered of Basement, ft. Comments
W-12301 Cabot Corp. Soc. 9 1974 185 15250 Barnett, 1975 Eagle Mills fm, 15100/90 quejta te sonP-731 1-.-USA T3N R25W training broken
pebbles of quart
& vocai metal.
W-14583 Mattle Kelly Simse Sec. 1980 26 14919 No published infor.
P-970 et al. Trustees T28 R22W nation.
No. 1
No W. Tenneco OIl Co., Soc. 31 1983 107 15362 No published Infor.
number USA*Fla. State T3N R25W mtion.
P.1105 Lease 3229F, 31-3
Okeechobee W-3739 Amerada Petroleum See. 5 1955 55 10838 Applin & Pre-Memsozol vol- 10750/8
P-237 Corp. Mare T368 R34E Applin, 1965 canic rocks Swaenson No. 1
W-12541 Shell Oil I Sec. 35 1974 60 11277 Barnett, 1975 Weathered dlabse 11220/57
P-710 Shell Scan 35-1 T358 RF26E
W-12542 Shell Oil 1 Sec. 9 1974 (KB)86 10767 Barnett, 1975 Weathered diabse 10642/103 Core samples 10764.
P-732 Joan M. Davis T3568 R35E 10772.67:191 t 15 grmnophyric dacite 1074529 m.y. (RbSr from porphyry feldspar by Shell)
Orange W4673 Warren Petroleum Sea. 21 1955 100 6589 ApplIn & granite 6550/39
P.230 Co. George Terry T238 R31E ApplIn, 1965 No. 1
W-10778 Texaco 1 Deseret Sec.15 1970 79 7119 Bamrnett, 1975 granite (Texaco, 7070/49
P.441 Farms T238 R33E Barnett did not examine)
1. Florida Bureau of Geology well number.
2. Unless otherwise Indicated, these are drill floor elevations (In feet above MSL).




FLORIDA DEEP WELL DATA (Primarily wells which penetrated basement, but including some significant wells which did not)
Depth to and
WellI and Completion Elev. of Total Depth Type of Basement Penetration
County Permit No. Well Name Location Date Well2, ft. of Well, ft. Reference Rock Encountered of Basement, ft. Comment
Osceola W-1014 Humble Oil & Re- Sec. 10 1946 62 8049 Applln, 1951 altered & veined 8035/14
P-8 fining Co. N. T278 R34E blotite granite Ray Carroll No. 1
Bass, 1969 altered & veined (Bass examined Original rock had low biotite granite core from 8042- temp. of cryst. Induced 8044) by high water-vapor pressure. Later
"catacasis" &
hydrothermal alteration. Age greater than 400
m.y. Is virtually
certain, probable age
of 530 m.y. is supported by ages from other
wells.
W-1411 Humble Oil & Re- Sec. 12 1946 86 8798 Applin, 1951 rhyolite 8740/58
P-31 fining Co. W. P. T31S R33E Hayman No. 1
Milton & 8781: whole rock Grasty, 1969 K-Ar age determination 173 : 4my
W-11341 Atlantic Richfield Sec. 24 1972 78 6898 Bamrnett, 1975 granite 6840/58 Cuttings 68806900:
P-643 2 Bronsons Inc. T278 R29E biotite granite pegmath.
W-11342 Atlantic Richfield Sec. 3 1972 86 7935 Bamrnett, 1975 granite 7890/45 Cuttings 7920-35: P-539 1 Bronsone Inc. T29S R31E blotite granite pegmatite.
Palm Beach W-1471 Humble Oil & Re- Sec. 35 1947 34 13375 Applin, 1951 TD in Jurassic (?).
P-47 fining Co. T43S R40E Tucson Corp. No. 1
W-12569 Shell 1 Gulf. Sec. 7 1975 30 16848 Bamett, 1975 igneous fragments in TO In lower part of
P-740 water 7.4 T468S R35E Lower Cretaceous basal basal elastic section, elastic section Lower Cret. Top, 16710-16770 basal clastics of 16440.
1. Florida Bureau of Geology well number.
2. Unless otherwise indicated, these are drill floor elevations (In feet above MSL).




FLORIDA DEEP WELL DATA (Prijriy wellse which penetreed 04imen, b~ Incl kding some igniftnl wetl which did not) U
Depth to and
Wel# end Completion Elev. of Tolw Depth Type of Pmeniri Penetraon
County Permit No. Well Name Location Datle Wed, fti. of Wel, ft. Reference Rock En oxointred of seenwit, ft. Corentw
PMsco W.11667 Atlantic Richfied See. 16 1973 (KB)88 900 Barnett, 1976 TD in koer pot of P.0A 1 J. B. Starkey T268 F17 bmeal Ol a Nadon, LOWer Cr5.
W-1239 nAmoco Prod. Co. Be0. 6 1974 134 7148 Barrnett, 1975 basal clastis 649634
P.743 1 Larkin Co. T258 R22E
8.4 weathered mugite 7129/19 diabasme (Jurassic)
W-12628 Amoco Prod. Co. Sec. 35 1974 10e 6646 Barnett, 1975 granite, late Precambrian 636/11 outings 66040-46:
P-742 1 Cummer 35-3 T238 R22E or Early Cambrian weathered & aeklniled blogi granite,
coarse oreined.
W.13028 Hary A. Holton See. 14 1976 (KB)60 9333 No pulled nform O
P475 No. 1 J.. T268 R17E matlon. "
Starkey 14.1
Pinellas W-1660 Coastal Petroleum Sea. 7 1948 13 11607 Applin, 1951 Did not reich beP-75 Co. E. C. Wright T30SS R17E ment TD In Lower No.1 Crt eou Or
W-6278 Califomla Co. 3 28'0532N 1963 57 10600 Bamrnett, 1975 Did not reach baseP-304 State Lease 224B 862'60'W ment TD in basal, detro meon,
Lower Cretceous.
Polk W-6741 Sun Oil I Soc. 19 1968 169 9670 Barnett, 1975 altered dlabase 9660/10
P-403 Shepard Dalry T325 R27E (Jurassic?)
Putnam W-1514 Sun Oil Co. & Soc. 19 1947 206 3328 Applin, 1961 Paleoolo quartalc 3320/8
P-58 Seaboard Oil Co.- TS R25E sandstone Q. 1. Roberta No. 1A
1. Florida Bureau of Geology well number.
2. Unles otherwin Indicated, these are drill floor elevation (in feet above MSL).




FLORIDA DEEP WELL DATA
(Primaily wells which penetrated basement, but Including some significant wallls which did not)
Depth to and
Well and Completion Elev. of Total Depth Type of Basement Penetration
County Permit No. Well Name Location Date Well2, ft. of Well, ft. Reference Rock Encountered of Basement, ft. Comments
W-1838 Sun Oil Co.- H.E. Sec. 37 1949 32 3892 Applin, 1951 volcanic ash & tuff 3873/19
P-96 Westbury et al. T11 IS R268E
No. 1 Bass, 1969 volcanicc tuff & 3876/16 Mineralogy consistent agglomerate, mostly with metarnm. of green- Z rhyolitlo composition schist fades or lower.
W-11530 Thayer & Davis Sec. 27 1972 34 665572 Bamett, 1975 rhyolite (not examined) 4426/1146
P-607 1 Johnson T11S R27E Malphure
St. Johns W-10653 Carolina Resources Sec. 70 1970 42 4850 Bamrnett, 1975 Paleozolc quartzitic 4830/20 0
P-435A 1 Cummer Co. TOS R29E sandstone Z
W-11084 Kerr McGee Corp. Sec. 35 1971 40 4583 Bameft, 1975 Paleozoic quartltic 4562/21
P-506 1 H. W. Mizell T7S R28E sandstone
St. Lucie W-4323 Amerada Petroleum Sec. 19 1957 32 12748 Applin & Pr.-Mesozoic meta- 12680/68 126680-725: weathered c
P-259 Corp. Cowles T3S R40E Applin, 1965 morphosed Igneous igneous rock.
Magazine No. 2 Intruslve rocks
Bass, 1969 diabase 12734/approx.
10 Z
metarn. rocks predom. 12744/approx. faulted against 0 amphibolite 4 overlying diabase.
age, based on analysis
of blotites 530 m.y.
MIlton, 1972 Report of Age determinations footnote 3.
W-13082 Amoco 1 Peacock Sec. 26 1975 26 12652 Bamett, 1975 no comments, had not
P-772 Fruit and Cattle T36S R39E been completed.
26-1
1. Florida Bureau of Geology well number.
2. Unless otherwise indicated, these are drill floor elevations (in feet above MSL).
3. Age determlnation-Amerada Petroleum Corp. Cowles Magazine No. 1




FLORIDA DEEP WEI. DATA
(Prtmarily wells which penel trated bement, but Including some aslOnirficanl wells which did nol)
Depth to and
Wolt and Completion Elev. of Total Depth Type of Basement Ptetration
County Permit No. Well Name Locatlon Date Weol, ft. of Well, ft. Reference Rock Encountered of Iasement, ft, Comments
Santa Rosa W-153l Getty Oil Co. Sec. 1 8pud 30 projected P.1097 State Leaae 2338 T25 R28W 6/1983 to 17800 No. 1
Suwannee W.1450 Bun Oil Co. Earl Sec. 31 1947 73 3161 Applin, 1951 Paleozolc black shale 3040/121 P-45 Odom No. 1 T56 R15E
W.1648 Sun Oil Co. J. H. Sec. 28 1947 162 3572 Applin, 1951 Paleozolo black shale 3500/72 m
P-57 T111ll No.1 T28 815E 5
W-1924, Sun OIl Co. A. S. Sec. 8 1949 96 3139 Applin, 1951 Paleozolo quartzftic 3163/3
1924A Russell T58 R15E sandstone
P-109 C
Sample Analyst Method Age 0 Depth Material 12734 Buasat Grsaty K.Ar 89.3t22my 12744 Granite " 226 t6my 224 t Smy
S Chloritized blotite from schist Base SriSr7 G 530 my
and quartz dlortte gneles
" K-Ar 399 my
Plagloolase from quartz dlorite 148 my
gnela
12748 Diorite Grasty x 308 t 5 m.y.
N Homblende In diorite Bass 470 m.y.
(amphlbollte) 503 m.y.
1. Florida Bureau of Geology well number.
2. Unless otherwise Indicated, these are drill floor elevations (in feet above MSL)




FLORIDA DEEP WELL DATA
(Primarily wells which penetrated basement, but Including some significant wells which did not)
Depth to and
Well1 and Completion Elev. of Total Depth Type of Basement Penetration
County Permit No. Well Name Location Date Well2, ft. of Well, ft. Reference Rock Encountered of Basement, ft. Comments
Suwannee,
(cont.) W-12246 Hunt Petr. 1 Sec. 16 1974 96 4520 Bamett, 1975 Paleozolc dark grey to 3726/284 coarsely micaceous,
P-724 C. R. Howes T28S R12E black shale thin as Interbeds.
Paleozolo quartzltic 4010/350 fine-med, white-grey, sandstone highly mlcaceous streaks
Paleozolc shale and 4360/150 red and brown stain. sandstone
qqartzlto sandstone & 4510/10 shale, Paleozolo
W-12247 Hunt Petr. 1 Sec. 5 1974 106 4496 Barnett, 1975 quartzItlc sandstone & 3640/390
P-723 T. P. Hurst T3SS RS13E shale, Paleozolo
black micaceous shale, 4030/486 greasy lustre, thin Paleozolo sands zones, some pyrltc streaks.
Taylor W-1677 Humble Oil & Sec. 12 1948 36 6254 Applin, 1951 Triasal? basaltic rock 6153/12 Underlies clastics of
P-865 Refining Co. T58 ROE TrIase? or Jur? age.
G. H. Hodges No. Triasslo? dlabase 6165/89
1 gabbro
W-2099 Gulf Oil Corp. Sec. 9 1949 41 5438 Applin, 1951 Trlassic? dlabase, prob. 5438/79 underlies clastice of P-116 Brooks Scanlon T188 ROE a lava flow Trdass? or Jur? age.
Inc., Block 42
No. 1
W-2106 Gulf Oil Corp. Sec. 18 1950 98 5243 Applin, 1951 Triasslc? dlabase 5200/43 underlies clastios of P-119 Brooks Scanlon T4S RSE gabbro TrIsse? or Jur? age.
Inc. Block 33
No. 1
1. Florids Bureau of Geology well number.
2. Unless otherwise Indicated, these are drill floor elevations (in feet above MSL).




FLORIDA DEEP WE1 DATA
(Primealy well which penetrated baement, but Including some ilgnifcent well* which did nol) 1
Depth to and
Woll' and Completion Klev. of Total Depth Type of Basement Penetration
County Permit No. Well Name Lation Date Well, ft. of Well, ft. Reference Rock Enountered of Baement, ft. Commenta
W.10018 Amoco Prod. 1 So, 12 1970 62 7036 arnett,1975 Paleosolo 5807/120
P-40 Canal Thr. Co. T3S6 PAE
Diabasee 6256/113
6417/247
0706/65
W-12697 Hunt Petr. 2 Sec. 34 1976 28 7475 Barnett, 1975 No comments, had not
P-774 Buckeye Cellulose TOS RIBE been completed.,
C
W.12781 Hunt Petr. 1 Sea. 22 1975 16 7503 No pubilehed Information.
P-776 Buckeye Cellulose TS8 RSE
W.14716 Amoco Frances Seo. 34 1980 113 6477 No published Information.
P.1015 Exnom 34-8 No. 1 T38 R29E
O
W.16445 Amoco Prod. Co. SO. 7 1983 113 9000 No published Information. I
P-1112 Buckeye Cellulose T48 ROE
7.4
Union No W-No. Getty Oil 1 Sea. 20 1973 139 3037 Barnett, 1975 Paleozolo (Getty) 3029/6 No samples available. MI
P-649 K. 0. Diake TSS R18E 0
W.11870 Getty Oil 1 Sec. 4 1973 156 3015 Bamrnett, 1975 No comments, samples
P-650 R. Billing 4.1 T8S R18E & loge not examined. i
W-11912 Gettay Oi 1 Seo. 31 1973 145 3061 Barnett, 1976 Paleozolc (Getty) 3048/16
P-680 W. Croft T48 R19E
1. Florida Bureau of Geology well number.
2. Unleess otherwise Indicated, these are drill floor elevations (In feet above MSL).




FLORIDA DEEP WELL DATA
(Primarily wells which penetrated basement, but including some significant wells which did not)
Depth to and
Well1 and Completion Elev. of Total Depth Type of Basement Penetration
County Permit No. Well Name Location Date Well2, ft. of Well, ft. Reference Rock Encountered of Basement, ft. Comments
Voluula W-1118 Sun Oil Co. Sec. 11 1946 48 5958 ApplIn, 1951 Homblende diorlte. 5910/48 P-19 Powell Land T178 R31E Bass, 1969 Transported material 5918/12 Base concludes that Co. No, 1 and/or weathered basement. the dlorite is probably a sill and
Less weathered, cuttings 6930/10 the country rock Z contain chlorite & meta-sedimentary. plagioclase, some quartz Total rock age: 480 0 & no hornblende. my. The diorite is older but not
quartz-bearing homblende 5940/10 greater than 624 my diorlte. old. Hornfela Is t prob. Precambrian O
hornblinde dlorite with 6950/5.5 or derived from a diabase-Ilke texture. sediment that was derived from Prec.
homfels derived from 5955.5/2.5 source. olayey volcanic-quartzose
s. C Milton & 5953-5954'; K-Ar: 480 my Grasty, 1969 (dated by H. Thomas, R. Marvin, P. Elmore, &
H. Smith, USGS). Z
W-1745A Grace Drilling Sec. 2 1949 44 5424 Applln, 1951 rhyolltic? volcanic rock 5403/21
P-78 Co. Retail TISS5 R30E Lumber Co. No. 1
Wakulia W-12114 Placid 011 Co. 1 Sec. 27 1973 99 OH 12242 Barnett, 1975 Eagle Mills hf. 11674/526
P-696 USA Unit 27-2 T2S R3W STH 11747
Paleozolo grey-black shale 12200/20 mloaceous, fissile
Diabase sill. 12220/22
1. Florida Bureau of Geology well number.
2. Unless otherwise Indicated, these are drill floor elevations (in feet above MSL).




FLORIDA DEEP WELL DATA
(Pnrimarilny wede Wbuc peerwaeld baument, but nck Og Some s ~ 'nt w*e wh.h did n~)
Depto to arid
We, and Copletion Elev of Total Depth Type of Basernt Penetrabon
County Permit No Well Name Location Date We08, it of Wed, It Reference Rock Encounteraed of Pase nt, It. Comment
Wallon W.11182 Coastal Prod. 1 Se. 9 1971 214 12340 Barnett, 1975 Me tamorphosed volcanic 12285/55 Core 12333-13340: 3' P-519 Brady Belcher T3N R21W sandstora & granule con- voic. granule congl.
glomerate. Cambnrian or & s, 3' aighd U. Precambrian metamorphoed red A green sh, 1 pebble
congi. a s.
Walon W.11374 Texas Gas Expl. Sec. 5 1972 294 12028 Barnett, 1975 Eagle Mille frn. 11389/442 P-587 1. International TSN R20W
Paper Co. Diabaae llls 11610/30 11997/31
W.11601 McCulloch 1 DS Sec. 24 1972 140 11533 Barnett, 1975 Eagle Mills fmn. 11422/111 cuttings at 11533;
P-612 Rudman 1 Indian T2N R19W very coame red es.
Crk Ranch
W.12309 CwterOil 4 Sc. 31 1974 43 14515 Barnett, 1975 granite 14480/35 cutting 14510-15: P*721 SL Joe Paper T 20W coarme red granite wah A weafhwed
blote grande
Puomaints.
Washinglon W*11398 A. Mosbacher et Sec. 20 1972 (KB)128 11692 Bamett, 1975 Cambrian or U. 11554/138 rhyo te, Arden,
P-549 al. 1 First Nat. TIN R15W Precambrian meta- 1974.
Bank of Akron arkose & qu rzte
W-11822 Rudman Resources Sec. 31 1973 153 11593 Barnett, 1975 Cambrian or U. 11480/113
P-644 1 FNB of Akron T2N R15W Precambrian meta31-2 arkose & quatite
W-12347 Hunt PetrL Sec. 11 1974 84 14044 Bamett, 1975 Eagle Mills frn. 10760/180
P.738 Internatlonal T4N R14W
Paper Co. Late Paleozok; 10040/240 Ordovician 11180/2864 1120-300: Sfphonohthe dt.
nta Jenlsm,
M. Ord. (Hurt plso).
1. Florida Bureau of Geology wel number.
2. Unless otevwlie indicated, these are drill floor elevations (in feet above MSL).




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'2017-03-09T11:24:59-05:00'
describe
'5266' 'info:fdaE20080623_AAAACEfileF20080623_AAAPZQ' 'sip-files00005.QC.jpg'
d74f712300f6a498b99dd9e82968fa15
a744dba78388d334f7dfb43f2e0f48c0491d8bc3
describe
'872248' 'info:fdaE20080623_AAAACEfileF20080623_AAAPZR' 'sip-files00005.tif'
b4ca6db019963dfbedf8b28e9653fc66
69a34da8b342de02a22d4c53dabf25f32da34330
describe
'285' 'info:fdaE20080623_AAAACEfileF20080623_AAAPZS' 'sip-files00005.txt'
6e0aae753e9955ad7da25c83fa4ea937
a5f45e0806dc951663ac29898fb575cda1a54857
'2017-03-09T11:24:39-05:00'
describe
'1937' 'info:fdaE20080623_AAAACEfileF20080623_AAAPZT' 'sip-files00005thm.jpg'
ee86484b2be96713d27aa325f3e59098
2c81e8b167c1ee901b1f8120a5eba7254c2c5117
'2017-03-09T11:25:32-05:00'
describe
'35018' 'info:fdaE20080623_AAAACEfileF20080623_AAAPZU' 'sip-files00006.jp2'
307a948c4b87d90fbb6dc416639616d7
789b610eae7af307714ef05c7714e3dcac8db7d2
'2017-03-09T11:28:24-05:00'
describe
'39037' 'info:fdaE20080623_AAAACEfileF20080623_AAAPZV' 'sip-files00006.jpg'
73444befdc7e996393c1eb0ad684868f
076d497a380e6014b970c8900ac9f0b33002aa70
'2017-03-09T11:28:51-05:00'
describe
'14181' 'info:fdaE20080623_AAAACEfileF20080623_AAAPZW' 'sip-files00006.pdf'
6e682489a56d1e7db4a2df7f4907f496
26649f56469cf44899a3b6cbfe038cae1756a4b3
'2017-03-09T11:27:45-05:00'
describe
'info:fdaE20080623_AAAACEfileF20080623_AAAPZW-norm-0' 'aip-filesF20080623_AAAPZW-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
'2017-03-09T11:29:20-05:00'
describe
'2017-03-09T11:27:47-05:00'
normalize
'27664' 'info:fdaE20080623_AAAACEfileF20080623_AAAPZX' 'sip-files00006.pro'
f18000cd7d525dfa501cd928a757e4ee
cf1aefb39e5ea35fbb0a9cbeb3f6bea960c721f1
'2017-03-09T11:28:13-05:00'
describe
'12892' 'info:fdaE20080623_AAAACEfileF20080623_AAAPZY' 'sip-files00006.QC.jpg'
0e4041bea6bf605e7703547146af7490
05ddeea0294397d11e6226d9819fcb7603be92df
'2017-03-09T11:27:12-05:00'
describe
'906580' 'info:fdaE20080623_AAAACEfileF20080623_AAAPZZ' 'sip-files00006.tif'
1dd4ac3e3a44917c07f8da5d9242b4a8
68304a4a687e94f38ffe45fd2a144a9c8f2cd45d
'2017-03-09T11:24:11-05:00'
describe
'914' 'info:fdaE20080623_AAAACEfileF20080623_AAAQAA' 'sip-files00006.txt'
0c3d342d189d5408d3d63998754062a9
7b730577eee5158c2607e5d9381d1def03d5ba59
'2017-03-09T11:25:44-05:00'
describe
'3416' 'info:fdaE20080623_AAAACEfileF20080623_AAAQAB' 'sip-files00006thm.jpg'
fd8297ec47cb54f665c6c1d421e85a7e
9185de9521ce1e7782fbdeb594cbdd4298548a81
'2017-03-09T11:28:32-05:00'
describe
'88301' 'info:fdaE20080623_AAAACEfileF20080623_AAAQAC' 'sip-files00007.jp2'
bf04e0f230ecf29f71281d799183b944
97c0a1b5e93ef0c545743603ea36b79fd7cc3fe4
'2017-03-09T11:24:52-05:00'
describe
'91333' 'info:fdaE20080623_AAAACEfileF20080623_AAAQAD' 'sip-files00007.jpg'
cc6f9d001bbb84fcd76149b2fd314ed5
dc66d080f459671e6ccc16fe3262846413d092eb
'2017-03-09T11:27:08-05:00'
describe
'38792' 'info:fdaE20080623_AAAACEfileF20080623_AAAQAE' 'sip-files00007.pdf'
2760967f5e9e901b08ee42ea347fd86f
e94c46ee0ea0632f667743b1ec2106887fd88179
'2017-03-09T11:24:23-05:00'
describe
'info:fdaE20080623_AAAACEfileF20080623_AAAQAE-norm-0' 'aip-filesF20080623_AAAQAE-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
'2017-03-09T11:29:23-05:00'
describe
'2017-03-09T11:24:25-05:00'
normalize
'33597' 'info:fdaE20080623_AAAACEfileF20080623_AAAQAF' 'sip-files00007.pro'
30286693ca2efc950d0e9b2cf0c9b9e1
b58031eb66c1cc54c3f00dceb145e4873584300b
describe
'28218' 'info:fdaE20080623_AAAACEfileF20080623_AAAQAG' 'sip-files00007.QC.jpg'
1139df6aa0f2c23f8e4e138d97f1f675
c4897f07fdf860318793b922a843ebc40ba22209
'2017-03-09T11:27:48-05:00'
describe
'886504' 'info:fdaE20080623_AAAACEfileF20080623_AAAQAH' 'sip-files00007.tif'
538a9edf2cade2d3036bfbfbe95378e4
a259c6f4eb6bcacd7e010ea0ab3e6b8fd8266736
describe
'1273' 'info:fdaE20080623_AAAACEfileF20080623_AAAQAI' 'sip-files00007.txt'
4bae673fca1e2a1290a2cecf737c9b8c
fe07f508fb238878ff3f81389da78ed630fa6644
'2017-03-09T11:28:28-05:00'
describe
'7226' 'info:fdaE20080623_AAAACEfileF20080623_AAAQAJ' 'sip-files00007thm.jpg'
8fe478575eab6af4eb4f4a85e640196f
deb693913422b223e44f50f39e493bea9bb2aa78
'2017-03-09T11:28:16-05:00'
describe
'170263' 'info:fdaE20080623_AAAACEfileF20080623_AAAQAK' 'sip-files00008.jp2'
0b8a2827908866d448656ea641e72c05
680322bd82c00cdb91902ddcbe7ac32bc70dfd70
describe
'165229' 'info:fdaE20080623_AAAACEfileF20080623_AAAQAL' 'sip-files00008.jpg'
08c31c54022d5d1425fb054cd8efa796
1b5af945ed44dfcd577fa1ca5a70c4dd724875ef
'2017-03-09T11:27:44-05:00'
describe
'73333' 'info:fdaE20080623_AAAACEfileF20080623_AAAQAM' 'sip-files00008.pdf'
3db300b6bcca2f30702445035cdae25a
b4b3e15cffb4bc1141eea853d9f7ac67d18f4069
'2017-03-09T11:29:07-05:00'
describe
'info:fdaE20080623_AAAACEfileF20080623_AAAQAM-norm-0' 'aip-filesF20080623_AAAQAM-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
'2017-03-09T11:29:21-05:00'
describe
'2017-03-09T11:29:09-05:00'
normalize
'65187' 'info:fdaE20080623_AAAACEfileF20080623_AAAQAN' 'sip-files00008.pro'
89d0d61cd9294ed79649c4adb774a458
74eb4444f78215d7704d921d25c0f1522283b18e
'2017-03-09T11:25:18-05:00'
describe
'49233' 'info:fdaE20080623_AAAACEfileF20080623_AAAQAO' 'sip-files00008.QC.jpg'
07af4f33433ca75f77f52886f7f40896
b723a476cfbca5d9e4044bb0234b413f5f7139d7
'2017-03-09T11:24:12-05:00'
describe
'907296' 'info:fdaE20080623_AAAACEfileF20080623_AAAQAP' 'sip-files00008.tif'
7cbd1ac0796671e04adb710ba91952c0
5a8d122cb5fe801e3a71e782ecf7cf5f15f7678c
'2017-03-09T11:28:27-05:00'
describe
'2520' 'info:fdaE20080623_AAAACEfileF20080623_AAAQAQ' 'sip-files00008.txt'
084996fa32dd467abd669d168aa59dce
a47aa7e8676d72c49051c867502f37f22811c87f
'2017-03-09T11:26:48-05:00'
describe
'12066' 'info:fdaE20080623_AAAACEfileF20080623_AAAQAR' 'sip-files00008thm.jpg'
059a6670980a6aa04cac57796f6ec9b4
fdd42fbed16cf77373182432cddb745a655275e5
'2017-03-09T11:25:06-05:00'
describe
'200529' 'info:fdaE20080623_AAAACEfileF20080623_AAAQAS' 'sip-files00009.jp2'
d3d791c1029d8c4dc094671af4b70dad
969dcfc59fc4338292213dc55f171df9a9d81a88
describe
'199927' 'info:fdaE20080623_AAAACEfileF20080623_AAAQAT' 'sip-files00009.jpg'
8c9587778983e65219822864b3c5f3a5
5f202c30c56741f5ba8d62571d7698990c5e15e8
'2017-03-09T11:28:17-05:00'
describe
'83595' 'info:fdaE20080623_AAAACEfileF20080623_AAAQAU' 'sip-files00009.pdf'
576089670e47af5058852be892544d5a
910b1ccb018d910b926cc7377760815fef9b55e3
'2017-03-09T11:27:58-05:00'
describe
'info:fdaE20080623_AAAACEfileF20080623_AAAQAU-norm-0' 'aip-filesF20080623_AAAQAU-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
'2017-03-09T11:29:25-05:00'
describe
'2017-03-09T11:28:00-05:00'
normalize
'78306' 'info:fdaE20080623_AAAACEfileF20080623_AAAQAV' 'sip-files00009.pro'
e5e982d3050fd90f83b9503d82ad7551
52a03f18db312c2a8b7e9f20f48cac6cd7515556
'2017-03-09T11:27:57-05:00'
describe
'60699' 'info:fdaE20080623_AAAACEfileF20080623_AAAQAW' 'sip-files00009.QC.jpg'
daa3c028af1b024fff879e564acaae03
90e4cf27178f44a991b19577d87d2b5b3c395c47
'2017-03-09T11:24:32-05:00'
describe
'888008' 'info:fdaE20080623_AAAACEfileF20080623_AAAQAX' 'sip-files00009.tif'
5a6ee9e59962413c801f96b8e7e72138
85476e9f81d2d9057a00ff420d547365f24374bd
'2017-03-09T11:28:15-05:00'
describe
'2908' 'info:fdaE20080623_AAAACEfileF20080623_AAAQAY' 'sip-files00009.txt'
45d94b1337ec9a86347d122a98b6ab9e
888e4be0072dbb2249a121877279d59f1f065996
'2017-03-09T11:27:50-05:00'
describe
'15388' 'info:fdaE20080623_AAAACEfileF20080623_AAAQAZ' 'sip-files00009thm.jpg'
6744866a5b8c010fbe8e408559cd9a85
1f002f5bfbb9a88ae3bcf4196d3545b3773f2a7a
describe
'227198' 'info:fdaE20080623_AAAACEfileF20080623_AAAQBA' 'sip-files00010.jp2'
c20b37ea17724784e6e7fbde6add70dc
f009466b102f2ae7a291eca19b563e4674f1a64d
'2017-03-09T11:24:50-05:00'
describe
'214806' 'info:fdaE20080623_AAAACEfileF20080623_AAAQBB' 'sip-files00010.jpg'
9e20112f8e9ab0b169e2944d81bd11f4
3f1f209c58e55a4bcfaf2c076683827f84d9cc49
'2017-03-09T11:26:34-05:00'
describe
'96440' 'info:fdaE20080623_AAAACEfileF20080623_AAAQBC' 'sip-files00010.pdf'
675c83783f50cee0e6fc6cdc53d791d0
35a42e8f2289c682e9fd9774d5d5072df199f185
'2017-03-09T11:25:09-05:00'
describe
'info:fdaE20080623_AAAACEfileF20080623_AAAQBC-norm-0' 'aip-filesF20080623_AAAQBC-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
'2017-03-09T11:25:11-05:00'
normalize
'87797' 'info:fdaE20080623_AAAACEfileF20080623_AAAQBD' 'sip-files00010.pro'
f2634ce0171fd936cd42215579f9c945
b64e7fe39aec1da0851e90a028fbb127fd3ea354
describe
'63886' 'info:fdaE20080623_AAAACEfileF20080623_AAAQBE' 'sip-files00010.QC.jpg'
7790a751efeedcdae2ae7881774e1388
ac70edf84dc9ff737afd392b0826764d05eefc6b
describe
'924536' 'info:fdaE20080623_AAAACEfileF20080623_AAAQBF' 'sip-files00010.tif'
6106a8a937153180a1f913eb274c6910
cf24439a2080facc28821520e764f934cdfd2669
describe
'3243' 'info:fdaE20080623_AAAACEfileF20080623_AAAQBG' 'sip-files00010.txt'
5c2f8ace947c78e9d7b276bd7c641f87
3c154d5f4b84800961750c51717cfaa58f348cf9
'2017-03-09T11:28:38-05:00'
describe
'14775' 'info:fdaE20080623_AAAACEfileF20080623_AAAQBH' 'sip-files00010thm.jpg'
edcdc3eadc598f1e5e610d775d9ea485
0e470978597874489e65d4d4c953d36d60f9e22a
'2017-03-09T11:26:38-05:00'
describe
'219683' 'info:fdaE20080623_AAAACEfileF20080623_AAAQBI' 'sip-files00011.jp2'
8d6176f6a35113f9941c700da242bf4c
958076549bcccbcf92bdfc74d960ddb0c807227a
'2017-03-09T11:24:02-05:00'
describe
'220816' 'info:fdaE20080623_AAAACEfileF20080623_AAAQBJ' 'sip-files00011.jpg'
911f8e1d853bccecebc3801cfa9fff18
76e1e883f494d611b6b6cb0e5449722f97ebaa37
describe
'92895' 'info:fdaE20080623_AAAACEfileF20080623_AAAQBK' 'sip-files00011.pdf'
a714f526d65253a64aadc6893dea1618
2cb2296ba0907422635a0b77574c9219c87aa7d4
'2017-03-09T11:26:40-05:00'
describe
'info:fdaE20080623_AAAACEfileF20080623_AAAQBK-norm-0' 'aip-filesF20080623_AAAQBK-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
normalize
'87835' 'info:fdaE20080623_AAAACEfileF20080623_AAAQBL' 'sip-files00011.pro'
329be952b661141d44658dce37a0a160
0672b2a99664ffb895c61e358505e1719de7c294
'2017-03-09T11:28:39-05:00'
describe
'67010' 'info:fdaE20080623_AAAACEfileF20080623_AAAQBM' 'sip-files00011.QC.jpg'
723cd95b93a0b7af05167992419a56fe
97229057d2fef73414d6977e6e50d1cd88304d92
'2017-03-09T11:28:01-05:00'
describe
'901972' 'info:fdaE20080623_AAAACEfileF20080623_AAAQBN' 'sip-files00011.tif'
d7946dfac87fa688c637a93bf16ecd17
4a1b03abaecd7c14c31e45931fce4b5953885c60
'2017-03-09T11:25:54-05:00'
describe
'3248' 'info:fdaE20080623_AAAACEfileF20080623_AAAQBO' 'sip-files00011.txt'
c9a458deb856c7751fd6700d2647f166
3f94aae823d642ac1fbbaae774069238d040a48a
'2017-03-09T11:24:53-05:00'
describe
'15585' 'info:fdaE20080623_AAAACEfileF20080623_AAAQBP' 'sip-files00011thm.jpg'
9ee5a51feffe7c0b88a74f3a0a85cea4
f1a052cb16a19a17b1789a6b2b1d47ead86f7115
describe
'212634' 'info:fdaE20080623_AAAACEfileF20080623_AAAQBQ' 'sip-files00012.jp2'
f568f954dbbf99928e540bbdbd02fbaf
339249040834599b5360c9734ef55ee915b8496a
describe
'202973' 'info:fdaE20080623_AAAACEfileF20080623_AAAQBR' 'sip-files00012.jpg'
2dbff47e909cc5c4911a7d00b911fe45
8d8eccd31a76fb0d981874f88fc76794b5c3eb88
'2017-03-09T11:28:43-05:00'
describe
'89345' 'info:fdaE20080623_AAAACEfileF20080623_AAAQBS' 'sip-files00012.pdf'
ecdf17fdb863a471d2c8123fe615dbdf
32812c53c9fe93bc068ebe00efc47b659a123cdf
'2017-03-09T11:26:26-05:00'
describe
'info:fdaE20080623_AAAACEfileF20080623_AAAQBS-norm-0' 'aip-filesF20080623_AAAQBS-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
'2017-03-09T11:26:28-05:00'
normalize
'82786' 'info:fdaE20080623_AAAACEfileF20080623_AAAQBT' 'sip-files00012.pro'
c2167567ae6b51f78fd64fcbb7e7a76d
3b6ed99ccb1babc725e6caac769ecfea876e56b7
'2017-03-09T11:26:39-05:00'
describe
'60775' 'info:fdaE20080623_AAAACEfileF20080623_AAAQBU' 'sip-files00012.QC.jpg'
293fda180f64cf92b8d5aa165e808b39
fcaaa8a19f7bd9919a679e7bcae1dc9ecf8ed2aa
describe
'921176' 'info:fdaE20080623_AAAACEfileF20080623_AAAQBV' 'sip-files00012.tif'
3ae1487b2d98278da2bbe8126e7b83ea
2b8bf41d0d5649ad5035704aad251ff9fc3eb3ff
'2017-03-09T11:24:57-05:00'
describe
'3070' 'info:fdaE20080623_AAAACEfileF20080623_AAAQBW' 'sip-files00012.txt'
6b73ddd3ab4cc822ca419e89569f497e
a047baf62e9ad8269ed1e0c8c527fbeae70a3218
describe
'14755' 'info:fdaE20080623_AAAACEfileF20080623_AAAQBX' 'sip-files00012thm.jpg'
e069988f45de65c01a81847fda15e664
f4d73c6bc8ad3e98615dda36a256962da36f885c
'2017-03-09T11:27:26-05:00'
describe
'204687' 'info:fdaE20080623_AAAACEfileF20080623_AAAQBY' 'sip-files00013.jp2'
ab099381a46acdf7ab12cead8a32aba9
f9eaa9a758aa3ea67954e7da78ca910f33fcdb57
'2017-03-09T11:25:59-05:00'
describe
'201171' 'info:fdaE20080623_AAAACEfileF20080623_AAAQBZ' 'sip-files00013.jpg'
9c92754f45ac9bacdd65b18c91126b8c
d1377d40b081adac93d0a4b4c6a022a86dccfabd
describe
'86380' 'info:fdaE20080623_AAAACEfileF20080623_AAAQCA' 'sip-files00013.pdf'
e553e5c58cbd36286611406311c8afa1
fc8d601cf7dc09b15ace97e1da417daf72bb9bda
'2017-03-09T11:26:29-05:00'
describe
'info:fdaE20080623_AAAACEfileF20080623_AAAQCA-norm-0' 'aip-filesF20080623_AAAQCA-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
'2017-03-09T11:26:31-05:00'
normalize
'80464' 'info:fdaE20080623_AAAACEfileF20080623_AAAQCB' 'sip-files00013.pro'
58655d67e6edf8cf35c3013996a1d8c8
5e8a3212584b7ac58ce8b422fbe1be2001a6f0e3
describe
'61238' 'info:fdaE20080623_AAAACEfileF20080623_AAAQCC' 'sip-files00013.QC.jpg'
aca34f86ee41b11eca28dc4724ab0043
32c4477a4b811434713d1ebc0cae72c3fa6dbfec
'2017-03-09T11:27:16-05:00'
describe
'901636' 'info:fdaE20080623_AAAACEfileF20080623_AAAQCD' 'sip-files00013.tif'
d941d494b3945ec4ee55bf921af7fccd
13df17d15c906ba1f8c2b6768bf69d32db5c5744
'2017-03-09T11:28:44-05:00'
describe
'2990' 'info:fdaE20080623_AAAACEfileF20080623_AAAQCE' 'sip-files00013.txt'
ab365907d0af0738090b57f6e6e5cfe3
ad3c94ef0c0ef5bdc418a62fb050347ec07d1c58
describe
'14932' 'info:fdaE20080623_AAAACEfileF20080623_AAAQCF' 'sip-files00013thm.jpg'
7bd721775e4d7e23e8a64c197d53ba23
d19231c0a11af452773499838bed0d7c4887be88
'2017-03-09T11:24:47-05:00'
describe
'221237' 'info:fdaE20080623_AAAACEfileF20080623_AAAQCG' 'sip-files00014.jp2'
6e28dc6aebf22f1fb5c1d3fb72aa5fc7
f8e4915e9607238ddc9aa94ae2245eee8167a811
'2017-03-09T11:24:38-05:00'
describe
'217875' 'info:fdaE20080623_AAAACEfileF20080623_AAAQCH' 'sip-files00014.jpg'
11e0694259038971425d020d95a08293
879d9b3e81b3f6fc506bd1c4cdd5c9d3588f8cab
describe
'94022' 'info:fdaE20080623_AAAACEfileF20080623_AAAQCI' 'sip-files00014.pdf'
6373d10476dd653e3dd7ded81051d081
5a818c5f15c9a83c703635ec6ec4fdafca849967
describe
'info:fdaE20080623_AAAACEfileF20080623_AAAQCI-norm-0' 'aip-filesF20080623_AAAQCI-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
'2017-03-09T11:29:24-05:00'
describe
'2017-03-09T11:24:27-05:00'
normalize
'86294' 'info:fdaE20080623_AAAACEfileF20080623_AAAQCJ' 'sip-files00014.pro'
19094716cf9ccfa6e8b3938c4b98bf4e
9101739e5ede6b979d7d07f798dcbea41e7f5ee2
'2017-03-09T11:24:22-05:00'
describe
'65498' 'info:fdaE20080623_AAAACEfileF20080623_AAAQCK' 'sip-files00014.QC.jpg'
32d05fa79389c16cd3ddad950c4c08c7
9a477a2f1df0a1372ea8bd782a6a003a707aa14f
'2017-03-09T11:28:59-05:00'
describe
'907068' 'info:fdaE20080623_AAAACEfileF20080623_AAAQCL' 'sip-files00014.tif'
93395ba41a34bf4188487b00658fbd35
f3ac4107a84e5bee66e586d3ff67dab1884cac97
'2017-03-09T11:28:11-05:00'
describe
'3179' 'info:fdaE20080623_AAAACEfileF20080623_AAAQCM' 'sip-files00014.txt'
bd54321aa69c58f2ee549280dbb5befc
1db29b518f7adb3b3b3966026ae83e357fc83b21
describe
'15411' 'info:fdaE20080623_AAAACEfileF20080623_AAAQCN' 'sip-files00014thm.jpg'
e2751eb1c2495252a3021e3bde96b0cb
309a0254aae46ae96533dbfb831d54785aaba3d1
'2017-03-09T11:29:16-05:00'
describe
'208086' 'info:fdaE20080623_AAAACEfileF20080623_AAAQCO' 'sip-files00015.jp2'
6d6d9921f6ab31e513b3e0c66914ed92
60ab618ce447cd6fa6544c67a450420b7348b93e
'2017-03-09T11:25:50-05:00'
describe
'207653' 'info:fdaE20080623_AAAACEfileF20080623_AAAQCP' 'sip-files00015.jpg'
f29c5440ddfae180ff32f94eac0e343e
693f6789801ccdd26c421af97fb3688ca0845835
describe
'88214' 'info:fdaE20080623_AAAACEfileF20080623_AAAQCQ' 'sip-files00015.pdf'
42509d3585c0ccdcd3900d9ec78b1e88
14b180bbd8b04076e0354e2750b13fd9ddeee100
'2017-03-09T11:28:20-05:00'
describe
'info:fdaE20080623_AAAACEfileF20080623_AAAQCQ-norm-0' 'aip-filesF20080623_AAAQCQ-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
'2017-03-09T11:28:22-05:00'
normalize
'83437' 'info:fdaE20080623_AAAACEfileF20080623_AAAQCR' 'sip-files00015.pro'
c8251e2492338914c070de717cd20016
f05960d327966e0e0fd38b098cbe3bfa3582aaa9
'2017-03-09T11:27:09-05:00'
describe
'63253' 'info:fdaE20080623_AAAACEfileF20080623_AAAQCS' 'sip-files00015.QC.jpg'
7390187316ac8b4ded64cbf5b0c77846
56e70e2a46112f6304982237e6f380c3542dfce3
'2017-03-09T11:29:03-05:00'
describe
'895496' 'info:fdaE20080623_AAAACEfileF20080623_AAAQCT' 'sip-files00015.tif'
cff25e863c7804e78448d0ea960074b9
fd455b20dfa796ed50ffe89febd1c780f025b4eb
'2017-03-09T11:28:19-05:00'
describe
'3086' 'info:fdaE20080623_AAAACEfileF20080623_AAAQCU' 'sip-files00015.txt'
33cdccd8e0a04b7fa6a4e923fbf508d6
9ca1b992550bcb412bf7123f70f5715f9086ca11
'2017-03-09T11:28:54-05:00'
describe
'15259' 'info:fdaE20080623_AAAACEfileF20080623_AAAQCV' 'sip-files00015thm.jpg'
b9b02dcb570b004a50ac099ed13f1e0c
eaa6d134ce7030a9aba8fa3812c4d94fca04d0aa
describe
'201782' 'info:fdaE20080623_AAAACEfileF20080623_AAAQCW' 'sip-files00016.jp2'
28088e9c41a791717a4c192b9f49ed24
69372411dbfe2f6da66b69449d5a5c1b12fc179c
'2017-03-09T11:25:45-05:00'
describe
'195059' 'info:fdaE20080623_AAAACEfileF20080623_AAAQCX' 'sip-files00016.jpg'
c0fad71ba4c280ee5fa025cb4cd6aa9d
720deb18390b3826f759881b3bd44ef3a29269db
'2017-03-09T11:25:58-05:00'
describe
'85319' 'info:fdaE20080623_AAAACEfileF20080623_AAAQCY' 'sip-files00016.pdf'
36ac99ee856b1d5603886761ad864512
b25fdfde34e08b214afc0f3f5314fa92543dc470
describe
'info:fdaE20080623_AAAACEfileF20080623_AAAQCY-norm-0' 'aip-filesF20080623_AAAQCY-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
'2017-03-09T11:29:26-05:00'
describe
'2017-03-09T11:26:25-05:00'
normalize
'78722' 'info:fdaE20080623_AAAACEfileF20080623_AAAQCZ' 'sip-files00016.pro'
c4498e94679fff382478861a0e6b23c9
7ab60bbc4789ab2bccb63d14b729f9aa87b8d06b
'2017-03-09T11:27:03-05:00'
describe
'58658' 'info:fdaE20080623_AAAACEfileF20080623_AAAQDA' 'sip-files00016.QC.jpg'
21c4f74632c2631770e3c00d84881a7e
a4c79df72a21a4b1788eb6256cf55e8c3669caeb
'2017-03-09T11:24:56-05:00'
describe
'916508' 'info:fdaE20080623_AAAACEfileF20080623_AAAQDB' 'sip-files00016.tif'
d5ac68973a81c8efa0101c08082ec9b3
ee19a399a59833ea26033165e692e689ad611091
describe
'2936' 'info:fdaE20080623_AAAACEfileF20080623_AAAQDC' 'sip-files00016.txt'
e7496c5da0a7800a0fb741fae5166a59
6ab985125dac282ba27fc58114aaa9982489c631
'2017-03-09T11:26:02-05:00'
describe
'14833' 'info:fdaE20080623_AAAACEfileF20080623_AAAQDD' 'sip-files00016thm.jpg'
9e402c80fcce8878de6c255aa8b5b2d3
ee3ae53cbd79a68fdaec9e55bb812629d5bf20d2
'2017-03-09T11:28:05-05:00'
describe
'219625' 'info:fdaE20080623_AAAACEfileF20080623_AAAQDE' 'sip-files00017.jp2'
4019139918a038cbf5cd89434997990d
d4d04c8d450a295cefc80d52baed780fbfea2319
'2017-03-09T11:25:30-05:00'
describe
'212154' 'info:fdaE20080623_AAAACEfileF20080623_AAAQDF' 'sip-files00017.jpg'
9cfc7a0bd29c52088c6988b7c0a7fefa
af194c0ad9f2397b49daf3e4297e75b877a64672
'2017-03-09T11:25:00-05:00'
describe
'92695' 'info:fdaE20080623_AAAACEfileF20080623_AAAQDG' 'sip-files00017.pdf'
de54eefa0363dc45bdb2496bfe554e4f
688ab84422032bdea99ef462342605ab7aca28ed
'2017-03-09T11:28:40-05:00'
describe
'info:fdaE20080623_AAAACEfileF20080623_AAAQDG-norm-0' 'aip-filesF20080623_AAAQDG-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
'2017-03-09T11:28:42-05:00'
normalize
'87297' 'info:fdaE20080623_AAAACEfileF20080623_AAAQDH' 'sip-files00017.pro'
90811d6ec9bf1596bec629fd05952448
ec51d0ed3598d75bf2c2535df4d555a274b7c200
'2017-03-09T11:24:33-05:00'
describe
'63599' 'info:fdaE20080623_AAAACEfileF20080623_AAAQDI' 'sip-files00017.QC.jpg'
f6099ee410646f85dc515b1a24ab8c61
bcc3ade2e1abfff9c05bfcc4b0110a48788fdd1d
'2017-03-09T11:27:02-05:00'
describe
'920388' 'info:fdaE20080623_AAAACEfileF20080623_AAAQDJ' 'sip-files00017.tif'
1e38043ad0889611138bee3076b628be
09feb78aa5d9ce78b961f0d53596a98bad4bca95
'2017-03-09T11:24:17-05:00'
describe
'3200' 'info:fdaE20080623_AAAACEfileF20080623_AAAQDK' 'sip-files00017.txt'
3e143cc69a491d50e400c3523925d346
8b713fc793408b77b9f7ec39a0c11faba892cb3e
describe
'15003' 'info:fdaE20080623_AAAACEfileF20080623_AAAQDL' 'sip-files00017thm.jpg'
b4873819f642a849c12a6567840de247
ac72f276a016dfc9245c69434161d8f4012ba709
'2017-03-09T11:25:03-05:00'
describe
'216282' 'info:fdaE20080623_AAAACEfileF20080623_AAAQDM' 'sip-files00018.jp2'
39740dd2da4fb25b9864e77325234370
9208b95dc96f73a7df3315513a746ee5f388ece6
'2017-03-09T11:24:28-05:00'
describe
'209126' 'info:fdaE20080623_AAAACEfileF20080623_AAAQDN' 'sip-files00018.jpg'
2dfa9d05899fcc39df189e2fe275a093
5033738b2a18302f8ac2b5720a511f29f6a55e19
'2017-03-09T11:24:01-05:00'
describe
'92414' 'info:fdaE20080623_AAAACEfileF20080623_AAAQDO' 'sip-files00018.pdf'
12522523cc3d835cf2589e57f3d80232
319db566951eecedeff0e2f2fb81ffb51d4e73d8
'2017-03-09T11:27:51-05:00'
describe
'info:fdaE20080623_AAAACEfileF20080623_AAAQDO-norm-0' 'aip-filesF20080623_AAAQDO-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
'2017-03-09T11:29:29-05:00'
describe
'2017-03-09T11:27:53-05:00'
normalize
'84758' 'info:fdaE20080623_AAAACEfileF20080623_AAAQDP' 'sip-files00018.pro'
d7c99577064257b22c4059579e669043
e7217f4a93a63fc27f07a9dfa13517a235c51b33
describe
'61935' 'info:fdaE20080623_AAAACEfileF20080623_AAAQDQ' 'sip-files00018.QC.jpg'
9a2464d12e3827dc91b50603e9303596
93928d379eae36c7428d1b4a39245053c64f3b0d
describe
'924568' 'info:fdaE20080623_AAAACEfileF20080623_AAAQDR' 'sip-files00018.tif'
1a94da8d36ac434ab1055240cf7a58e1
75fdfaf13854a34c602b12a303eb18bedd0b733e
describe
'3124' 'info:fdaE20080623_AAAACEfileF20080623_AAAQDS' 'sip-files00018.txt'
4c800af8e3a8a366a636fac09759715c
a2a179b06311d3e4d1fa7d3f26ced985e14d00fe
describe
'14756' 'info:fdaE20080623_AAAACEfileF20080623_AAAQDT' 'sip-files00018thm.jpg'
416968ee30ac8a6d61072cefa389e857
711824ac3ee3789341838cf1da50bb70a9e580f2
describe
'217364' 'info:fdaE20080623_AAAACEfileF20080623_AAAQDU' 'sip-files00019.jp2'
2ba822af4a59a0fa79b1ad3fd1a9a98d
bd0d61b43613e495f50cb02282e4228c2b9cf851
describe
'210923' 'info:fdaE20080623_AAAACEfileF20080623_AAAQDV' 'sip-files00019.jpg'
f84ed3559a5dd1ebc9f08cd9b4d5b13b
d24aaa3743622686bb5009f6839ba59860fbee9c
describe
'92691' 'info:fdaE20080623_AAAACEfileF20080623_AAAQDW' 'sip-files00019.pdf'
4c5c535983ff5e89bc66688ed803c59b
e8df374ff7b1635dacb7a70118109568f483a2f7
describe
'info:fdaE20080623_AAAACEfileF20080623_AAAQDW-norm-0' 'aip-filesF20080623_AAAQDW-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
'2017-03-09T11:28:03-05:00'
normalize
'85024' 'info:fdaE20080623_AAAACEfileF20080623_AAAQDX' 'sip-files00019.pro'
ab02cdb569a735f94c77a700f1c4592f
337b1e259c326f5d9c582fcfb68a8582d90f408e
describe
'63936' 'info:fdaE20080623_AAAACEfileF20080623_AAAQDY' 'sip-files00019.QC.jpg'
9a00228dcb10776f9620ce76712af757
53b3af6fbeefd779bd7f99944ce3cf133c658b4d
'2017-03-09T11:24:46-05:00'
describe
'919460' 'info:fdaE20080623_AAAACEfileF20080623_AAAQDZ' 'sip-files00019.tif'
9135f425cbfc1d13650cbc1ca9f3a23e
5866e0002b9af77eefd09e715c3389b73e7c5045
'2017-03-09T11:26:07-05:00'
describe
'3136' 'info:fdaE20080623_AAAACEfileF20080623_AAAQEA' 'sip-files00019.txt'
9785766d5bf4da3b95caf9c5bc374b2c
410d0bb3b8a27407e8b461db615c8edeec25dd56
describe
'15334' 'info:fdaE20080623_AAAACEfileF20080623_AAAQEB' 'sip-files00019thm.jpg'
5a242e566f6f0ab140da11ec5dd40c6f
b64fc191555b95ceb1f59047499388e34452bb33
'2017-03-09T11:27:15-05:00'
describe
'222230' 'info:fdaE20080623_AAAACEfileF20080623_AAAQEC' 'sip-files00020.jp2'
82a29e979990e252ee3554c1a9a42b1b
d58f62f16e0500897dece3ca6a43a18971eb13f3
describe
'213606' 'info:fdaE20080623_AAAACEfileF20080623_AAAQED' 'sip-files00020.jpg'
881ece978888d6e406cd513abdac33dc
707c8142eae372d24255e88b821f7dd3d26390af
describe
'95339' 'info:fdaE20080623_AAAACEfileF20080623_AAAQEE' 'sip-files00020.pdf'
f0030d4ecad743a7fffce6ec692f12fb
58b788ba843051c8029074a84e154684ca09259c
'2017-03-09T11:26:13-05:00'
describe
'info:fdaE20080623_AAAACEfileF20080623_AAAQEE-norm-0' 'aip-filesF20080623_AAAQEE-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
'2017-03-09T11:29:22-05:00'
describe
'2017-03-09T11:26:15-05:00'
normalize
'85468' 'info:fdaE20080623_AAAACEfileF20080623_AAAQEF' 'sip-files00020.pro'
06153b9a3a1ee6d7180374f2db120a72
6284ffaf8313505fd6b4441cd6f65826a5ef9bfd
'2017-03-09T11:28:12-05:00'
describe
'63299' 'info:fdaE20080623_AAAACEfileF20080623_AAAQEG' 'sip-files00020.QC.jpg'
e8dffc4bb4da56a2ed8d11d79e1cee67
9dbeef2f3d5d73e9700e942a46af580bba115c5f
describe
'921256' 'info:fdaE20080623_AAAACEfileF20080623_AAAQEH' 'sip-files00020.tif'
c57eefccb68e070d4b4380094c8cf5ff
bdeabe45f551bf337d485d1b631d69efe7119c0f
describe
'3175' 'info:fdaE20080623_AAAACEfileF20080623_AAAQEI' 'sip-files00020.txt'
80a45b22901263e9144b170d8fab752a
aaee9979ad44ccc2ab8f611296284bf8e82331a1
describe
'14836' 'info:fdaE20080623_AAAACEfileF20080623_AAAQEJ' 'sip-files00020thm.jpg'
df9c7aae1f6b0b855dd44bcf8154cea1
03038874d0e10c041fa2471c0ca2d49da60d57b6
'2017-03-09T11:24:16-05:00'
describe
'213554' 'info:fdaE20080623_AAAACEfileF20080623_AAAQEK' 'sip-files00021.jp2'
50d12198256628ef51f585b10f9a72c3
f41e05d08aeb0e5f0ef8ef222f58b4a1624417e1
describe
'214526' 'info:fdaE20080623_AAAACEfileF20080623_AAAQEL' 'sip-files00021.jpg'
f82bf4fb5823e775c9010fb43fc30a6b
7b389d6ae0fd62740d7f27df616fefc9469b624b
describe
'91222' 'info:fdaE20080623_AAAACEfileF20080623_AAAQEM' 'sip-files00021.pdf'
3a6f9a761d0c6f7483c2ed919d8f8731
10c9e13138258b36f8513484a944f3edd660ce4e
describe
'info:fdaE20080623_AAAACEfileF20080623_AAAQEM-norm-0' 'aip-filesF20080623_AAAQEM-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
'2017-03-09T11:26:18-05:00'
normalize
'85363' 'info:fdaE20080623_AAAACEfileF20080623_AAAQEN' 'sip-files00021.pro'
797305182f499a6b9b3bd9e0884a46cb
9602ffcaddf46d5664d3d33d77414ef0edf3106b
describe
'65079' 'info:fdaE20080623_AAAACEfileF20080623_AAAQEO' 'sip-files00021.QC.jpg'
c0f06d6bcd9e36b4b13ec7d85dd77765
7f7e7a523de99267c28e4a4dc1a7d56be10e1551
'2017-03-09T11:25:08-05:00'
describe
'901784' 'info:fdaE20080623_AAAACEfileF20080623_AAAQEP' 'sip-files00021.tif'
0bb3faaf4b16414ae66a75e097a2b8cb
20fcd15eef7a748c6337613175bca431f7150b7c
'2017-03-09T11:25:29-05:00'
describe
'3141' 'info:fdaE20080623_AAAACEfileF20080623_AAAQEQ' 'sip-files00021.txt'
843ba7fcd4193d44c48525bc32c1bb64
49fc57712267f01b3a0b7ee8e50b0eeccd773c6d
describe
'15592' 'info:fdaE20080623_AAAACEfileF20080623_AAAQER' 'sip-files00021thm.jpg'
24be76d975a62bc17fc05a9ee936e7f0
53f959c7e54d54f76bc5261ff1d2cf986ccb7779
describe
'212686' 'info:fdaE20080623_AAAACEfileF20080623_AAAQES' 'sip-files00022.jp2'
5a4c33f56c0c26e593e72de3a45644b4
2d3ea460e1e559a09b2b7513d354e70b8a6c91e0
describe
'203920' 'info:fdaE20080623_AAAACEfileF20080623_AAAQET' 'sip-files00022.jpg'
5a7a3dea9d80ed11ce2da885db4dbe39
7a82ea52a57cc8da21b4475e918c09527f7dad9c
'2017-03-09T11:26:58-05:00'
describe
'89895' 'info:fdaE20080623_AAAACEfileF20080623_AAAQEU' 'sip-files00022.pdf'
254e3e14df488feb2d8d2ad58362c44e
dd9608f34176a3c082ffdb15ad3621987e2f0f12
'2017-03-09T11:29:10-05:00'
describe
'info:fdaE20080623_AAAACEfileF20080623_AAAQEU-norm-0' 'aip-filesF20080623_AAAQEU-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
normalize
'82892' 'info:fdaE20080623_AAAACEfileF20080623_AAAQEV' 'sip-files00022.pro'
800f4a72706c3e0496cdb582b4096741
9e11707bbbc02b636915911a30dafb57b8a62545
describe
'60356' 'info:fdaE20080623_AAAACEfileF20080623_AAAQEW' 'sip-files00022.QC.jpg'
56b6d8bb45383fb54a22d20d34a82fbf
b469531127ad16600ec799d5f071b274b3be4270
'2017-03-09T11:25:39-05:00'
describe
'921440' 'info:fdaE20080623_AAAACEfileF20080623_AAAQEX' 'sip-files00022.tif'
869dcc8c59a5239c3afe35977d02f7f9
4bb6d6d36a53955bd98ae099619972cbe0eccad6
describe
'3154' 'info:fdaE20080623_AAAACEfileF20080623_AAAQEY' 'sip-files00022.txt'
9101f0eb281542bc2518b787faa85c57
567dbe1d6b4d3d050fa67bd9620d650bf2e7b2f5
'2017-03-09T11:25:07-05:00'
describe
'14393' 'info:fdaE20080623_AAAACEfileF20080623_AAAQEZ' 'sip-files00022thm.jpg'
5df23bd363e1a9c750a6d5f81325b591
6d800ffe92f9b4d87237faedc4916b42f1f29113
describe
'215732' 'info:fdaE20080623_AAAACEfileF20080623_AAAQFA' 'sip-files00023.jp2'
373f7e16d0074af75e9185dc4df6b297
d0179d527110061157c5bb212eb94b6d1a4bf2b5
describe
'213849' 'info:fdaE20080623_AAAACEfileF20080623_AAAQFB' 'sip-files00023.jpg'
f1d6a46eef8b2b76d10b81f23fcbb03d
5908e7430f0b43d562c849d038e994bfd8d0ae8a
describe
'91441' 'info:fdaE20080623_AAAACEfileF20080623_AAAQFC' 'sip-files00023.pdf'
16510185f73bbdb6a73222754f65e289
ea67eb58fd54da2cb300caee50c6c7fd898332cc
'2017-03-09T11:24:04-05:00'
describe
'info:fdaE20080623_AAAACEfileF20080623_AAAQFC-norm-0' 'aip-filesF20080623_AAAQFC-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
normalize
'84635' 'info:fdaE20080623_AAAACEfileF20080623_AAAQFD' 'sip-files00023.pro'
ec2f5e791cd4d3182997b139f8e4bd7d
e59b0f853ceb00a65c61c377c3d22c4d14d503c7
'2017-03-09T11:25:31-05:00'
describe
'63829' 'info:fdaE20080623_AAAACEfileF20080623_AAAQFE' 'sip-files00023.QC.jpg'
461d5f042aee07a912b54963f53e1a9b
a5f54f903edb6bf1724e7e0db0c44a7fd9ed3f6a
describe
'901484' 'info:fdaE20080623_AAAACEfileF20080623_AAAQFF' 'sip-files00023.tif'
3464c8e1050f2eeb76bba3695585ff8c
6d3e28df8f637991ac283aab7af35c7b6c6b884c
describe
'3102' 'info:fdaE20080623_AAAACEfileF20080623_AAAQFG' 'sip-files00023.txt'
386b404d17dcf646f7857c139b5adf7a
683796e0feb8da47a9449cc89915b334dcc6ade9
describe
'15584' 'info:fdaE20080623_AAAACEfileF20080623_AAAQFH' 'sip-files00023thm.jpg'
f33ff1a505b80f18ba61af153d88c25d
6c0c5b9ba71d1d660286afe80bf4a527560caf9e
describe
'214053' 'info:fdaE20080623_AAAACEfileF20080623_AAAQFI' 'sip-files00024.jp2'
dc1e6a8ed811599ccd109f281adcaf85
a61f4c7ff67e27ced03a47ea60d24894fa117665
describe
'205821' 'info:fdaE20080623_AAAACEfileF20080623_AAAQFJ' 'sip-files00024.jpg'
b8fb0138ce1b0a300629b44c8555af64
0c057148003e6ffb9e778cb694eb84d069e7ecc9
describe
'91167' 'info:fdaE20080623_AAAACEfileF20080623_AAAQFK' 'sip-files00024.pdf'
a86e05deb237d928388f197afb705d5e
2f8b05871de7eba00459d40f8eb33ce3ce09f52e
'2017-03-09T11:24:54-05:00'
describe
'info:fdaE20080623_AAAACEfileF20080623_AAAQFK-norm-0' 'aip-filesF20080623_AAAQFK-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
normalize
'82817' 'info:fdaE20080623_AAAACEfileF20080623_AAAQFL' 'sip-files00024.pro'
d40f3b616cf2759d232bf2871207a9a5
560308cac20170f3c644be5cdad344da83cc5fe7
describe
'61685' 'info:fdaE20080623_AAAACEfileF20080623_AAAQFM' 'sip-files00024.QC.jpg'
da8fe1d592992006e8d549700c21d9c3
cc1f13599b72025bf08c18ddfe4b35a9c41a2889
describe
'924096' 'info:fdaE20080623_AAAACEfileF20080623_AAAQFN' 'sip-files00024.tif'
0f6d8cfcc159046bf8eff45a21fe5233
6a3f3c43db5e71db6aca20e05382b88b51d8f658
describe
'3078' 'info:fdaE20080623_AAAACEfileF20080623_AAAQFO' 'sip-files00024.txt'
f42be2c15550441b8cada7c202803f80
c03a6dbf56b9fa13232853e330acd47adf823c5e
describe
'14670' 'info:fdaE20080623_AAAACEfileF20080623_AAAQFP' 'sip-files00024thm.jpg'
5149ea595341ff1c07ec379ded24e116
8777d9360eecda6b6f6cef3d1f5845c8e39546a1
'2017-03-09T11:26:55-05:00'
describe
'215751' 'info:fdaE20080623_AAAACEfileF20080623_AAAQFQ' 'sip-files00025.jp2'
a501aa043dea7741d1365b3bbac42c13
66da3d3ca7952423b48930fa0336d5e42631498c
'2017-03-09T11:24:21-05:00'
describe
'214595' 'info:fdaE20080623_AAAACEfileF20080623_AAAQFR' 'sip-files00025.jpg'
d3100ff07e2243da595d5ec2be6dbac8
07d6f4fe42fc278e710f2e0f3cf44fe7beaeedc1
'2017-03-09T11:26:37-05:00'
describe
'91700' 'info:fdaE20080623_AAAACEfileF20080623_AAAQFS' 'sip-files00025.pdf'
93cf7ee0193077dc0089ef9e2583df95
1c6e49025023b68ec93b61cfcbde1de784f3b5f8
'2017-03-09T11:26:03-05:00'
describe
'info:fdaE20080623_AAAACEfileF20080623_AAAQFS-norm-0' 'aip-filesF20080623_AAAQFS-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
'2017-03-09T11:26:05-05:00'
normalize
'85672' 'info:fdaE20080623_AAAACEfileF20080623_AAAQFT' 'sip-files00025.pro'
ea992433bb83265def9d10ea2037c62d
337e661bec6543bbd3f6c5bc86783aa7410de3bd
describe
'64158' 'info:fdaE20080623_AAAACEfileF20080623_AAAQFU' 'sip-files00025.QC.jpg'
0516c4f6821d2228512193f32dc162cc
3bf9eca3eab2bb5df7aa3dc307819fa48c3cffb4
describe
'902292' 'info:fdaE20080623_AAAACEfileF20080623_AAAQFV' 'sip-files00025.tif'
90f46e573ed1292a3b92e364869a3d30
da2c062422376b2286022a920ce3b61f94eb9607
describe
'3138' 'info:fdaE20080623_AAAACEfileF20080623_AAAQFW' 'sip-files00025.txt'
a12727249b850c9d1305759621a6c7b2
35e71bca97d1aefb6c8e8751319dbcd968e12b6b
describe
'15512' 'info:fdaE20080623_AAAACEfileF20080623_AAAQFX' 'sip-files00025thm.jpg'
7bfa8e980fe21d5af39d234cba358b1b
7ed424f0c1b86aa46f858453b3faac416a0a8ff6
describe
'220219' 'info:fdaE20080623_AAAACEfileF20080623_AAAQFY' 'sip-files00026.jp2'
98d534a820b62ae021c4fdadf1254fa4
3fee773878481b5fbfe34f90928092ef0ebce771
'2017-03-09T11:25:16-05:00'
describe
'211061' 'info:fdaE20080623_AAAACEfileF20080623_AAAQFZ' 'sip-files00026.jpg'
e51ec2965c408a72ec2fd65a58415c93
c777eebf2e683ddf948198f1577d1e9058e004b0
'2017-03-09T11:26:43-05:00'
describe
'94014' 'info:fdaE20080623_AAAACEfileF20080623_AAAQGA' 'sip-files00026.pdf'
89760f73f6abcd95a4093b2196acfe81
b66e1e2b755944af302b7322fdb70359621cd648
'2017-03-09T11:26:00-05:00'
describe
'info:fdaE20080623_AAAACEfileF20080623_AAAQGA-norm-0' 'aip-filesF20080623_AAAQGA-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
normalize
'87068' 'info:fdaE20080623_AAAACEfileF20080623_AAAQGB' 'sip-files00026.pro'
765a2cfb69a97ce637d974d52587f53b
3c06c4521a997e0015393d574a82f35b566fd73b
'2017-03-09T11:25:51-05:00'
describe
'63758' 'info:fdaE20080623_AAAACEfileF20080623_AAAQGC' 'sip-files00026.QC.jpg'
0fe96454056e98a40d8a065c6f0f77bb
51ade9f3a83b53ed69c76937bfbe05da224a701a
describe
'924432' 'info:fdaE20080623_AAAACEfileF20080623_AAAQGD' 'sip-files00026.tif'
cb3dd7a62e4b713cb8208c62f36c75fc
a8fde436faab7be0a10667515e9cbd9c2536045c
describe
'3197' 'info:fdaE20080623_AAAACEfileF20080623_AAAQGE' 'sip-files00026.txt'
4cd364e9b0da22cfc6056292100a3a56
3b989aa17dab9810a379472eaaaf8ff3cad4523b
describe
'15127' 'info:fdaE20080623_AAAACEfileF20080623_AAAQGF' 'sip-files00026thm.jpg'
40402c802139885c42318978689a8f42
3b6dc1486d0d5ab6bb4ee7a7d4cdf433d758935a
describe
'225578' 'info:fdaE20080623_AAAACEfileF20080623_AAAQGG' 'sip-files00027.jp2'
83244500f0e7f797ee4af2569d7d4051
f70bf5614e42a67f2ea74e583df205146a6b3ee4
describe
'220654' 'info:fdaE20080623_AAAACEfileF20080623_AAAQGH' 'sip-files00027.jpg'
477f7c20371e547a272b95c2b5c7ce36
d53f729f0d87c517320119c2a646972e1818ae8f
'2017-03-09T11:25:53-05:00'
describe
'96352' 'info:fdaE20080623_AAAACEfileF20080623_AAAQGI' 'sip-files00027.pdf'
90f57a89a6000ebf45c8237d271c47a6
3a26fa71223f3c2d99581d662275fcce976fe7ac
describe
'info:fdaE20080623_AAAACEfileF20080623_AAAQGI-norm-0' 'aip-filesF20080623_AAAQGI-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
'2017-03-09T11:28:49-05:00'
normalize
'91409' 'info:fdaE20080623_AAAACEfileF20080623_AAAQGJ' 'sip-files00027.pro'
5a4a4453e4c7ac7f02792558d70829de
c2bd2724c684c17865010ad276976752f4a5ff72
'2017-03-09T11:28:53-05:00'
describe
'65633' 'info:fdaE20080623_AAAACEfileF20080623_AAAQGK' 'sip-files00027.QC.jpg'
90d8b4eaa6d173b56c376b9b6427a9b7
3c08c2b48e1d3c39003367e7ac49b5e126341af0
describe
'919632' 'info:fdaE20080623_AAAACEfileF20080623_AAAQGL' 'sip-files00027.tif'
91b3642bd31f089421707a1af61a42df
dad138e00d7c673b9527f52b01ed85d4574f622c
'2017-03-09T11:28:26-05:00'
describe
'3337' 'info:fdaE20080623_AAAACEfileF20080623_AAAQGM' 'sip-files00027.txt'
7d58926d297649d23f3a8ec14bb6213e
0c4a7f3c397f55c97d5f1b5eb354110748ed7585
describe
'15471' 'info:fdaE20080623_AAAACEfileF20080623_AAAQGN' 'sip-files00027thm.jpg'
70f1e1072ad577633b88ef1747757763
df0511c98282df001f35d26e26965e281c49e463
'2017-03-09T11:25:49-05:00'
describe
'230751' 'info:fdaE20080623_AAAACEfileF20080623_AAAQGO' 'sip-files00028.jp2'
163c8ed04a4325e0f5b7c4617cbea78e
410bd685b8e131874ad0a4945fdc7486069f624b
'2017-03-09T11:25:40-05:00'
describe
'223245' 'info:fdaE20080623_AAAACEfileF20080623_AAAQGP' 'sip-files00028.jpg'
d279fc113b74716a8bde25034df8201a
73c9dd41725508a3045b6bf96feb9d422f6bf1a1
describe
'99188' 'info:fdaE20080623_AAAACEfileF20080623_AAAQGQ' 'sip-files00028.pdf'
41ddeaa5feb1e185a0d1971e9b4ce74d
92d2a9d217749e79c641140d6e5b897ad67ac009
'2017-03-09T11:24:41-05:00'
describe
'info:fdaE20080623_AAAACEfileF20080623_AAAQGQ-norm-0' 'aip-filesF20080623_AAAQGQ-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
'2017-03-09T11:29:18-05:00'
describe
'2017-03-09T11:24:44-05:00'
normalize
'91504' 'info:fdaE20080623_AAAACEfileF20080623_AAAQGR' 'sip-files00028.pro'
e398951e069c1c68160f7e02f1387fdc
719b22b1b85a39c19bd0d2c57b9ecb582a717ddb
describe
'64836' 'info:fdaE20080623_AAAACEfileF20080623_AAAQGS' 'sip-files00028.QC.jpg'
c617423a3e13a563b18f96d8b4bf5655
4ee1ae8128b33a1d5f7e1a3d29fb03470372caaf
'2017-03-09T11:27:13-05:00'
describe
'923520' 'info:fdaE20080623_AAAACEfileF20080623_AAAQGT' 'sip-files00028.tif'
d1a7c62d7aebe67316bdb3e90582445f
8e679a74b8e2e2f876878e7b3c3cdc0ec4a2b114
describe
'3365' 'info:fdaE20080623_AAAACEfileF20080623_AAAQGU' 'sip-files00028.txt'
e8950f0b930c53a6393296f3e4cdb12e
155d365eec4f1bccef7acd3971ea7d2f9fe7ea48
describe
'15067' 'info:fdaE20080623_AAAACEfileF20080623_AAAQGV' 'sip-files00028thm.jpg'
89924b061061579462d20794958cc02e
819c26148dc5e54f8d7933fb6b1d5c511a5150c1
describe
'226563' 'info:fdaE20080623_AAAACEfileF20080623_AAAQGW' 'sip-files00029.jp2'
4b6c6c07c1cafd83da87245a67a8f5f0
6586920b98700d0020db62dea430ad7baccfb308
'2017-03-09T11:25:12-05:00'
describe
'223774' 'info:fdaE20080623_AAAACEfileF20080623_AAAQGX' 'sip-files00029.jpg'
9f5278196635748ff571a9de54e65498
b4048741c80f10d9ebe84b27c5546896deefaaee
describe
'96951' 'info:fdaE20080623_AAAACEfileF20080623_AAAQGY' 'sip-files00029.pdf'
30ebb849b3766cfe82d0ea3c3838d49a
888c766cad5d7145c7e7156fc2f8c4effed33d56
'2017-03-09T11:26:53-05:00'
describe
'info:fdaE20080623_AAAACEfileF20080623_AAAQGY-norm-0' 'aip-filesF20080623_AAAQGY-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
normalize
'90305' 'info:fdaE20080623_AAAACEfileF20080623_AAAQGZ' 'sip-files00029.pro'
bd37deb35fc323a968e464afb3409192
f9c784191590d4b828824df76d2c608ce04e03b6
describe
'66411' 'info:fdaE20080623_AAAACEfileF20080623_AAAQHA' 'sip-files00029.QC.jpg'
28ea0e17a851a1e901130783ec8970d9
0929b0f53abad3fb380d6529fbf06c3c61e9c320
describe
'907884' 'info:fdaE20080623_AAAACEfileF20080623_AAAQHB' 'sip-files00029.tif'
ec8645fda72779faca4e2c64175b9ea9
9ce14ab5b6e5c85edcafd403fc3b67212e52e4c2
describe
'3302' 'info:fdaE20080623_AAAACEfileF20080623_AAAQHC' 'sip-files00029.txt'
9f266ea1a845fb5edd6d7701b0a86cb4
805ad3431fea9c501bc30b2e1c28487f7d672e99
describe
'15422' 'info:fdaE20080623_AAAACEfileF20080623_AAAQHD' 'sip-files00029thm.jpg'
b061d5cb47230b5fce5a9f1bd463a36c
6fca1aca2900a501f73136d5fab495ccad37cf3a
describe
'218584' 'info:fdaE20080623_AAAACEfileF20080623_AAAQHE' 'sip-files00030.jp2'
c0b1b339878a15a23aeef213575ebcda
fef6e620ac5824f622e9327bc4921d065b5115a7
'2017-03-09T11:29:02-05:00'
describe
'209159' 'info:fdaE20080623_AAAACEfileF20080623_AAAQHF' 'sip-files00030.jpg'
b68a947c2b9b474dc8e35b04eb51af1d
43fc1678084d5efca760389a3427a7f2c5313eae
'2017-03-09T11:25:57-05:00'
describe
'92783' 'info:fdaE20080623_AAAACEfileF20080623_AAAQHG' 'sip-files00030.pdf'
cfd3dd632fc16a3abe9b6e61ac3a27e8
dc5f41b709f07bb8b9bbc5e6c89dd32586708999
'2017-03-09T11:25:01-05:00'
describe
'info:fdaE20080623_AAAACEfileF20080623_AAAQHG-norm-0' 'aip-filesF20080623_AAAQHG-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
normalize
'84449' 'info:fdaE20080623_AAAACEfileF20080623_AAAQHH' 'sip-files00030.pro'
9c72e02ce01bb79db4520c98b297c78d
23559e993c4b9ce7103c70d1f6f38a79d0f2f8a2
'2017-03-09T11:28:23-05:00'
describe
'63655' 'info:fdaE20080623_AAAACEfileF20080623_AAAQHI' 'sip-files00030.QC.jpg'
1552db970cf102b395f5b6b5ff08690d
0f744030cd607c85ee86c69654ae9f4c45f1a3ff
describe
'910848' 'info:fdaE20080623_AAAACEfileF20080623_AAAQHJ' 'sip-files00030.tif'
ec2ae870e20fac1e1a1f24f0878796c8
5e30e73ab785f2c0fd52d45d930aca99bbdb2efb
describe
'3119' 'info:fdaE20080623_AAAACEfileF20080623_AAAQHK' 'sip-files00030.txt'
5475047b531fb69e0b6ab24456100028
a119afe972e7374a15ff134aefe57f7516d46995
describe
'14826' 'info:fdaE20080623_AAAACEfileF20080623_AAAQHL' 'sip-files00030thm.jpg'
0cab19736891935ef27a321147c4565f
43bff1393ab8ed9732b9b3721dadbe254c7adac9
'2017-03-09T11:26:47-05:00'
describe
'213530' 'info:fdaE20080623_AAAACEfileF20080623_AAAQHM' 'sip-files00031.jp2'
66e9b4f5133e1a491fade1762b4e0a94
fe5fcccbb4166427d527fabb1e2aa3222ba1bd44
describe
'208031' 'info:fdaE20080623_AAAACEfileF20080623_AAAQHN' 'sip-files00031.jpg'
24e51c33ded9923e5f371da182b5d650
6f3c5b70fd68487d35a1b1845b11bb08677cb348
describe
'90647' 'info:fdaE20080623_AAAACEfileF20080623_AAAQHO' 'sip-files00031.pdf'
89d33f8e6df10aec4a808aff31526a85
f965c84f64245eff5a9a438722beac7bd14631ac
'2017-03-09T11:29:13-05:00'
describe
'info:fdaE20080623_AAAACEfileF20080623_AAAQHO-norm-0' 'aip-filesF20080623_AAAQHO-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
'2017-03-09T11:29:15-05:00'
normalize
'84036' 'info:fdaE20080623_AAAACEfileF20080623_AAAQHP' 'sip-files00031.pro'
ae76c94906b15071aca5df0284c8ef42
26f311db42d068604deeab7a28966d606f626520
describe
'62314' 'info:fdaE20080623_AAAACEfileF20080623_AAAQHQ' 'sip-files00031.QC.jpg'
df526e0de7d737310e34db9a55505249
07db865255ec0780c67bc01efb50b0e8e54a69d2
describe
'924072' 'info:fdaE20080623_AAAACEfileF20080623_AAAQHR' 'sip-files00031.tif'
c71ef101694fa7ceaf761e8f19bce163
8ecba760fc7e09745c25c4353f71253e22d325e0
describe
'3147' 'info:fdaE20080623_AAAACEfileF20080623_AAAQHS' 'sip-files00031.txt'
f1d9ed57aacba7ff56469117712613a3
bb959fad4fb966a5066acdbc3f5bd8b7cec414d9
describe
'14980' 'info:fdaE20080623_AAAACEfileF20080623_AAAQHT' 'sip-files00031thm.jpg'
dbb6c3d64d5ef64c72b2f6c84913e352
65c8cec91a6f09c8782380fb361d359acf283cb8
describe
'219372' 'info:fdaE20080623_AAAACEfileF20080623_AAAQHU' 'sip-files00032.jp2'
4d3b333ce30e824be4cadf0e1858f33d
d0c8d05281580a8e7ade2a14b5af7629b8ca9146
describe
'209278' 'info:fdaE20080623_AAAACEfileF20080623_AAAQHV' 'sip-files00032.jpg'
a6150a3a6bc301e4d940a5d1382f84ae
2582c33ab642bdf67c69767d6a44f9a52e3526c0
describe
'92885' 'info:fdaE20080623_AAAACEfileF20080623_AAAQHW' 'sip-files00032.pdf'
3542702ab895a4720cc51573ee7efd10
698daa2ffec8a8932920ec9c483fd2116b7b9480
describe
'info:fdaE20080623_AAAACEfileF20080623_AAAQHW-norm-0' 'aip-filesF20080623_AAAQHW-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
'2017-03-09T11:25:56-05:00'
normalize
'86096' 'info:fdaE20080623_AAAACEfileF20080623_AAAQHX' 'sip-files00032.pro'
adf376cf85517c89106a2e24194468fa
0978af05828d074651bf51ce65c34e276583765c
'2017-03-09T11:28:04-05:00'
describe
'64265' 'info:fdaE20080623_AAAACEfileF20080623_AAAQHY' 'sip-files00032.QC.jpg'
59d1dc436740ae80fb0f82789f21c7c0
ffff999c1ee30d72451c1eeaf91b9f858acefa6d
describe
'922568' 'info:fdaE20080623_AAAACEfileF20080623_AAAQHZ' 'sip-files00032.tif'
b8a399032c6c719847e0d4b08b6f467d
6968a90b324616b18e488377f36d0e464d05cfd5
describe
'3190' 'info:fdaE20080623_AAAACEfileF20080623_AAAQIA' 'sip-files00032.txt'
2648bae8f8d843de5651c4a3afb55e42
30bb36fa059ea180c35db6fe1b1f3a3807c97e22
describe
'14916' 'info:fdaE20080623_AAAACEfileF20080623_AAAQIB' 'sip-files00032thm.jpg'
6b4be8ff3b091aa27d2a8d93d9169096
5015f82a36f6e41386efd89383bc4c7e40bc0e3f
describe
'207221' 'info:fdaE20080623_AAAACEfileF20080623_AAAQIC' 'sip-files00033.jp2'
a9e13975a88f27a1539529ebdca31e9b
9615fa6d17ac0dbdca472f6ac5192adcae576cf8
describe
'200061' 'info:fdaE20080623_AAAACEfileF20080623_AAAQID' 'sip-files00033.jpg'
026d7838b2f690d168cffff1e401b451
2c81cd991ae90296e0de271ec70d36e9ce854e04
describe
'86749' 'info:fdaE20080623_AAAACEfileF20080623_AAAQIE' 'sip-files00033.pdf'
ad20dfba2e13e48fed9a6c8df758110e
225f35f28fc732382b3e20e3beae8fad9f9daf35
'2017-03-09T11:27:17-05:00'
describe
'info:fdaE20080623_AAAACEfileF20080623_AAAQIE-norm-0' 'aip-filesF20080623_AAAQIE-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
'2017-03-09T11:27:19-05:00'
normalize
'80846' 'info:fdaE20080623_AAAACEfileF20080623_AAAQIF' 'sip-files00033.pro'
12b7aec0051e22c19e8d96eecdffb9ad
073e64d8aceda994637fc57c79f1984fc32e1acc
describe
'61261' 'info:fdaE20080623_AAAACEfileF20080623_AAAQIG' 'sip-files00033.QC.jpg'
61b3862b120e124e719b504f6fbf2dd4
10f6f6c60595778f57e8ee0cbac0266a0fe40d5a
describe
'922892' 'info:fdaE20080623_AAAACEfileF20080623_AAAQIH' 'sip-files00033.tif'
2a6c5fbfe9cf9ca72292ae9a4c206b76
5d711c12a2cd2250cbb5f792c74fb07e954f294f
'2017-03-09T11:28:29-05:00'
describe
'2970' 'info:fdaE20080623_AAAACEfileF20080623_AAAQII' 'sip-files00033.txt'
d4927eccb3b7e1c2be2a16394037adb2
903369fb0b1fbe2f47025b8ff3d52a5801b59806
describe
Invalid character
WARNING CODE 'Daitss::Anomaly' Invalid character
'14657' 'info:fdaE20080623_AAAACEfileF20080623_AAAQIJ' 'sip-files00033thm.jpg'
92043190e49b07176f6d8b9644474575
7f55e985f2b2960ffbef5540d364a30e071c0853
'2017-03-09T11:25:33-05:00'
describe
'233462' 'info:fdaE20080623_AAAACEfileF20080623_AAAQIK' 'sip-files00034.jp2'
cd0ffa963f20839b29b1ce9227de4855
a546e072eac5e8743d8dd8f4bb8add0fb5b219cf
describe
'230879' 'info:fdaE20080623_AAAACEfileF20080623_AAAQIL' 'sip-files00034.jpg'
62001aad1670386fcc1948c04b32cc76
54a4d7cb64960315291ac4b4967a746700d79933
describe
'99055' 'info:fdaE20080623_AAAACEfileF20080623_AAAQIM' 'sip-files00034.pdf'
2db6d28f3c521ad77f12ea3478301fb0
c336d980b2d0cb77fc552cb734c4d807fd60faed
describe
'info:fdaE20080623_AAAACEfileF20080623_AAAQIM-norm-0' 'aip-filesF20080623_AAAQIM-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
'2017-03-09T11:25:42-05:00'
normalize
'91783' 'info:fdaE20080623_AAAACEfileF20080623_AAAQIN' 'sip-files00034.pro'
007ae1cd7214440a04c93455eda68dfa
e98ff50c804cf89f909acf4332926fdef197d207
describe
'68754' 'info:fdaE20080623_AAAACEfileF20080623_AAAQIO' 'sip-files00034.QC.jpg'
717de191d20d91f487469de3df62fc66
3d1386f3cda515627aec00ffb5ff419909ed8833
describe
'888928' 'info:fdaE20080623_AAAACEfileF20080623_AAAQIP' 'sip-files00034.tif'
92a9fb1eb3a2446dd8eb8f9984590e7d
ef5109fce674e693ad994addec298275cc34e9bd
describe
'3374' 'info:fdaE20080623_AAAACEfileF20080623_AAAQIQ' 'sip-files00034.txt'
9dd010bbce53241b2d12cf0453003e5e
993ad264321fabedb2cad2284043988dc8169ad9
describe
'16604' 'info:fdaE20080623_AAAACEfileF20080623_AAAQIR' 'sip-files00034thm.jpg'
fb79177d19eafd3351939cd5ff323ffb
2cc6d4de4fd70cc6479189de333c668eff8f1923
describe
'218096' 'info:fdaE20080623_AAAACEfileF20080623_AAAQIS' 'sip-files00035.jp2'
b6ade9118a20bf748548ac274b842515
fdcbf5e34e2975d3e0a7f3e8f431e00db3a85e4f
describe
'213893' 'info:fdaE20080623_AAAACEfileF20080623_AAAQIT' 'sip-files00035.jpg'
9c5aa8e1a2a8b219e30686ef3d1bef9b
7cde9670eab4c8b26f9a9e4524d738e1d0154654
describe
'92034' 'info:fdaE20080623_AAAACEfileF20080623_AAAQIU' 'sip-files00035.pdf'
79bfd8dd38133508ff46ad0d72eb068b
40e6a2f542b99b4c75bd919afc08af27d91dbeff
describe
'info:fdaE20080623_AAAACEfileF20080623_AAAQIU-norm-0' 'aip-filesF20080623_AAAQIU-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
normalize
'85748' 'info:fdaE20080623_AAAACEfileF20080623_AAAQIV' 'sip-files00035.pro'
c3598ed4ff2972d2706394c8a0f37b17
dc6a73b4dd1733c04fe4384fd99339970ede81ef
describe
'63835' 'info:fdaE20080623_AAAACEfileF20080623_AAAQIW' 'sip-files00035.QC.jpg'
3c49f7c8c4c2f1801fe324b3e3854d6a
cf9190d10e0e5537101cdea5c041ec9ef6286e91
describe
'921800' 'info:fdaE20080623_AAAACEfileF20080623_AAAQIX' 'sip-files00035.tif'
25f96611e8bfa2829352aa72ae1461b4
0b90ce1da8fc7b1c7e2261e6de35cb4425e33ef4
'2017-03-09T11:24:13-05:00'
describe
'3151' 'info:fdaE20080623_AAAACEfileF20080623_AAAQIY' 'sip-files00035.txt'
df17c01d778968a4cbffa0eaf31a1147
ccc7cb0b497e9c8a2f9e05ab296f115d6b236631
describe
Invalid character
Invalid character
'15419' 'info:fdaE20080623_AAAACEfileF20080623_AAAQIZ' 'sip-files00035thm.jpg'
2a3f7fc5d5e0a067423a693907792b7d
c7ced5cc7e6fc6c3508ecaf50f1e446a3064cdcb
describe
'225484' 'info:fdaE20080623_AAAACEfileF20080623_AAAQJA' 'sip-files00036.jp2'
216b5fface73c07a5ca6a794c6be72c8
7d908df4f6763917075850d69a6982b19d554d05
describe
'218384' 'info:fdaE20080623_AAAACEfileF20080623_AAAQJB' 'sip-files00036.jpg'
6ef9f960b7c21f6c3b35e83f0360c02c
95bbe8db5fe82f2d2b5171c486f708f17f25e45b
describe
'95575' 'info:fdaE20080623_AAAACEfileF20080623_AAAQJC' 'sip-files00036.pdf'
0cfe77b2bf75bdd54cb019e80c3405e7
0deeef1cd4df7dfd26555f9b08424b2118c2fee0
'2017-03-09T11:28:36-05:00'
describe
'info:fdaE20080623_AAAACEfileF20080623_AAAQJC-norm-0' 'aip-filesF20080623_AAAQJC-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
normalize
'89314' 'info:fdaE20080623_AAAACEfileF20080623_AAAQJD' 'sip-files00036.pro'
eff2f2a0774cb4719462d07390016594
dcf179b2a4943c9655bd6d6796c6261f280b315f
describe
'66006' 'info:fdaE20080623_AAAACEfileF20080623_AAAQJE' 'sip-files00036.QC.jpg'
a5ae8d5b252a9739f2f5447b0844bdbb
4b3a2a4c69772e58a30ba1a9d0088731f3d9bf13
describe
'893872' 'info:fdaE20080623_AAAACEfileF20080623_AAAQJF' 'sip-files00036.tif'
cc5f9ae1269a54d4c7681cc4876996fe
4984fad2cb96421810801880c1c461fb214d2c27
'2017-03-09T11:25:36-05:00'
describe
'3290' 'info:fdaE20080623_AAAACEfileF20080623_AAAQJG' 'sip-files00036.txt'
61b3b96bed63b316e2c8427b86bf8552
ad030db5c58e6f8514b31386433d23c0c9d336c2
describe
'15829' 'info:fdaE20080623_AAAACEfileF20080623_AAAQJH' 'sip-files00036thm.jpg'
1395133d35d8e9c0b383748466fe44a5
3bdd6ab6974dbdb8851dd67b1d90bb0f1cf45648
'2017-03-09T11:24:15-05:00'
describe
'220114' 'info:fdaE20080623_AAAACEfileF20080623_AAAQJI' 'sip-files00037.jp2'
7e69482a214db2f9a9ab44c415ba515a
b49fd911b5fad0c4b20c6902dfb07842e3b22e77
describe
'212969' 'info:fdaE20080623_AAAACEfileF20080623_AAAQJJ' 'sip-files00037.jpg'
c8d72eece3eb8f131fda8f813e145051
818ff603bf9dc28707bdb8024ac8c54fdf65dc4e
describe
'93319' 'info:fdaE20080623_AAAACEfileF20080623_AAAQJK' 'sip-files00037.pdf'
bfbf39b9b8d6248a0699c1dad63c160a
d68c7c1836a9acdabc3b4e82cc45c49ee98ad054
'2017-03-09T11:26:35-05:00'
describe
'info:fdaE20080623_AAAACEfileF20080623_AAAQJK-norm-0' 'aip-filesF20080623_AAAQJK-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
normalize
'86108' 'info:fdaE20080623_AAAACEfileF20080623_AAAQJL' 'sip-files00037.pro'
1204d10e9b430e0bf420b9b1b5a53df0
2426b5617f42352d8e7640144e21521cd2b24c58
describe
'63171' 'info:fdaE20080623_AAAACEfileF20080623_AAAQJM' 'sip-files00037.QC.jpg'
2b7d18f9f2160c1d09a31c94f08d98ed
f230de118c3b6cc4d94c405babc75e6989f2a0bc
describe
'921764' 'info:fdaE20080623_AAAACEfileF20080623_AAAQJN' 'sip-files00037.tif'
da38dd9f8489987bb22c55357f52d8f3
bbeece30d32f7703d3b769f4561af12d8f58ff75
describe
'3159' 'info:fdaE20080623_AAAACEfileF20080623_AAAQJO' 'sip-files00037.txt'
a602278c70d4893e15bdd31cdd34af42
1545acfdd0353cb0e3d0cc3a200e53b1870fc53e
describe
'15298' 'info:fdaE20080623_AAAACEfileF20080623_AAAQJP' 'sip-files00037thm.jpg'
956eaa7a119fab3cf7cc4dcf53dd484f
1d50e7e708cba458d176d0ec209cd4a7fc1241d9
'2017-03-09T11:25:26-05:00'
describe
'211092' 'info:fdaE20080623_AAAACEfileF20080623_AAAQJQ' 'sip-files00038.jp2'
2e4a42cccab51e3afa29e3ee09ef3a63
13ef9293a1cbc7e324b6dc09e4034ddf906bc9b2
describe
'204249' 'info:fdaE20080623_AAAACEfileF20080623_AAAQJR' 'sip-files00038.jpg'
55a83eb3076486807a8ea79ede2d5bb6
b95ec112fb037841c1d9be74a9d4fe3dcd91c3b7
describe
'89539' 'info:fdaE20080623_AAAACEfileF20080623_AAAQJS' 'sip-files00038.pdf'
256eefa2b9b1b9cc5d1e28d9f92f1109
dfeca6aad2e202e5e25525d8a8f2f46d87e64c18
describe
'info:fdaE20080623_AAAACEfileF20080623_AAAQJS-norm-0' 'aip-filesF20080623_AAAQJS-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
'2017-03-09T11:26:50-05:00'
normalize
'82587' 'info:fdaE20080623_AAAACEfileF20080623_AAAQJT' 'sip-files00038.pro'
a87b37a90a190be2a5471ebf8e4ec4c1
4827457d9ad7328f03c62659ea3aabcb0821f1fc
describe
'62256' 'info:fdaE20080623_AAAACEfileF20080623_AAAQJU' 'sip-files00038.QC.jpg'
5b1f9dba3db12543a351a63283703281
9fa54b19e797f4e7802fd39519dfc60384202bfd
describe
'908464' 'info:fdaE20080623_AAAACEfileF20080623_AAAQJV' 'sip-files00038.tif'
9f3c4da6e83cdb85918ea563a7b2b8aa
86c3eede99dec8435266462f55acd6f606d97be4
'2017-03-09T11:27:22-05:00'
describe
'3055' 'info:fdaE20080623_AAAACEfileF20080623_AAAQJW' 'sip-files00038.txt'
5cddc75b2ea54dea31d44dfe228e5724
7a4bc3000a5f9bf2a598fe6f797bdec30f3062e7
describe
'15114' 'info:fdaE20080623_AAAACEfileF20080623_AAAQJX' 'sip-files00038thm.jpg'
bffc239210731a06dca5a0e9c0f6ec6f
0dd3c966bfb688c71ca228e9a7ea6bb6eec3dd04
describe
'208531' 'info:fdaE20080623_AAAACEfileF20080623_AAAQJY' 'sip-files00039.jp2'
ecbc43621e9cff32f65d61e29abbb9e1
93cb62ed581d000613d66c26bcbf65777bd41966
'2017-03-09T11:24:14-05:00'
describe
'207678' 'info:fdaE20080623_AAAACEfileF20080623_AAAQJZ' 'sip-files00039.jpg'
59f8f921ade4c301deb11efe777c5d91
3200b28e2e23ae3afa1f138358d1fb14bf92433b
describe
'89623' 'info:fdaE20080623_AAAACEfileF20080623_AAAQKA' 'sip-files00039.pdf'
73dff03bbe89e283393c03617ba4ba48
dbb217c567c539bfaa278a4a4e3b78042af3030c
'2017-03-09T11:26:32-05:00'
describe
'info:fdaE20080623_AAAACEfileF20080623_AAAQKA-norm-0' 'aip-filesF20080623_AAAQKA-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
'2017-03-09T11:29:27-05:00'
describe
normalize
'83222' 'info:fdaE20080623_AAAACEfileF20080623_AAAQKB' 'sip-files00039.pro'
fa22930144c5f38e572bfe387b10fac6
b446cbb9e9005998adcf015b8b6dd180c7a90d6b
describe
'61733' 'info:fdaE20080623_AAAACEfileF20080623_AAAQKC' 'sip-files00039.QC.jpg'
59103b9e0e7b847baf2ccd28bcd411a7
6ec61b87313481bb5e3568690ff9748336baeb91
'2017-03-09T11:27:20-05:00'
describe
'888096' 'info:fdaE20080623_AAAACEfileF20080623_AAAQKD' 'sip-files00039.tif'
a6e42d0911cf9612460379923dfdd62c
609db724fddf679c64641ff1a960e2837ef80009
describe
'3115' 'info:fdaE20080623_AAAACEfileF20080623_AAAQKE' 'sip-files00039.txt'
81f233d263356f15aeb848f7634ffff6
d0f169252c2c109ba949b58d748525eb1aadd146
'2017-03-09T11:24:37-05:00'
describe
'15007' 'info:fdaE20080623_AAAACEfileF20080623_AAAQKF' 'sip-files00039thm.jpg'
1b405e57255b982e94b30f0658594e04
0db5a563ef6edc8980eeac0034a739ac5554777c
describe
'234756' 'info:fdaE20080623_AAAACEfileF20080623_AAAQKG' 'sip-files00040.jp2'
b1e71c72ab1b75f7f9a499a13326d458
a801ec1c5ebb062f5388a96de2281d874b06c06a
describe
'227593' 'info:fdaE20080623_AAAACEfileF20080623_AAAQKH' 'sip-files00040.jpg'
9607d2bfa8445aa18da5c8702a38dc3d
0734aeaeba522a143bc650d11e524aadd0a16da3
describe
'101738' 'info:fdaE20080623_AAAACEfileF20080623_AAAQKI' 'sip-files00040.pdf'
33a40115ee065ae5377d2bbc82e71029
a012bbecba3c7a77cb85873719465c3e5cd40671
describe
'info:fdaE20080623_AAAACEfileF20080623_AAAQKI-norm-0' 'aip-filesF20080623_AAAQKI-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
normalize
'91821' 'info:fdaE20080623_AAAACEfileF20080623_AAAQKJ' 'sip-files00040.pro'
246c9ef479759975fe45a107c717f08b
8ca6a4b6ea51fc7c526fde934c65d9feb386cf73
describe
'68067' 'info:fdaE20080623_AAAACEfileF20080623_AAAQKK' 'sip-files00040.QC.jpg'
4e6eb59652e9a92028fbadfd8d82e26e
a128b85a0d8e290d3988bdb9abd485c3f996af4e
describe
'908204' 'info:fdaE20080623_AAAACEfileF20080623_AAAQKL' 'sip-files00040.tif'
adf5ad34a07f668dc06f81b0a2cee34f
21c28aeb59819c05ee806e69ee7365127984e4ab
describe
'3391' 'info:fdaE20080623_AAAACEfileF20080623_AAAQKM' 'sip-files00040.txt'
5cff96b5eb340e46ed2b589ae5493324
b1d4e74d10516023d2deaae1034b9e6d4db727e2
describe
'15676' 'info:fdaE20080623_AAAACEfileF20080623_AAAQKN' 'sip-files00040thm.jpg'
32ebb5af348d9ba513505dc2f13f55bd
b3c7809e096b7a96b5683c0be25eb796f335b400
describe
'223545' 'info:fdaE20080623_AAAACEfileF20080623_AAAQKO' 'sip-files00041.jp2'
3713fc9c48f3d63a4f7b827ffd56faa5
fc5f3d131cbbc5db4682b18174bc16976a2d7a9b
describe
'214869' 'info:fdaE20080623_AAAACEfileF20080623_AAAQKP' 'sip-files00041.jpg'
813ed3d6c2241faa62856b91c853f0dd
9616768db476e58907ed028f4f57936e0c2ffb93
describe
'94552' 'info:fdaE20080623_AAAACEfileF20080623_AAAQKQ' 'sip-files00041.pdf'
49d9a11bb9e8f7ac51512d2c7fba2104
4a74bf055bdeff027f981edbad36aad51da405e2
'2017-03-09T11:25:34-05:00'
describe
'info:fdaE20080623_AAAACEfileF20080623_AAAQKQ-norm-0' 'aip-filesF20080623_AAAQKQ-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
normalize
'87066' 'info:fdaE20080623_AAAACEfileF20080623_AAAQKR' 'sip-files00041.pro'
c17975f05f1393fc38c2a0282c582bd0
fbb06d5f8c811567b7bcdd50fa3c948475b7c37d
'2017-03-09T11:28:06-05:00'
describe
'63937' 'info:fdaE20080623_AAAACEfileF20080623_AAAQKS' 'sip-files00041.QC.jpg'
bd4d0b6bef644171a372a6cb042642da
da5cf452d0e08105b1b187c7145d4d684d0a8a70
describe
'921232' 'info:fdaE20080623_AAAACEfileF20080623_AAAQKT' 'sip-files00041.tif'
a27faece318381cf2282fd5aa942cc06
ef08e603c7f322070506b1216dbc6e0f1e40d265
describe
'3212' 'info:fdaE20080623_AAAACEfileF20080623_AAAQKU' 'sip-files00041.txt'
a9e1aaa4db10dbd673f48a88291592cd
bcdcd46c943ab65786b1faabce3dee2fe297e859
describe
'15023' 'info:fdaE20080623_AAAACEfileF20080623_AAAQKV' 'sip-files00041thm.jpg'
7c2d02545b951f7be4c34ed18429a28e
c0d460b9197a1ebc817c6df177485ef790b58bd6
'2017-03-09T11:26:45-05:00'
describe
'224404' 'info:fdaE20080623_AAAACEfileF20080623_AAAQKW' 'sip-files00042.jp2'
2fbdf7c7029cf86585128651528bcf01
5e214591959aba9187bf0bed0dbb0384cce404dd
describe
'217310' 'info:fdaE20080623_AAAACEfileF20080623_AAAQKX' 'sip-files00042.jpg'
5e24febf3b2249d456571e756180c451
69e08d9bcc51921e6bbb28a15d1b8758a9e65355
describe
'96615' 'info:fdaE20080623_AAAACEfileF20080623_AAAQKY' 'sip-files00042.pdf'
6500f2a3791724373ab097e7e7b5cc16
f2cb1b0cc3889caeb5b8d43105a3deae7018be48
describe
'info:fdaE20080623_AAAACEfileF20080623_AAAQKY-norm-0' 'aip-filesF20080623_AAAQKY-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
normalize
'89362' 'info:fdaE20080623_AAAACEfileF20080623_AAAQKZ' 'sip-files00042.pro'
31f666aaf6c1274678dcc12679dcb9a2
d2cb8033a2695bbe21925699bb5e910ad0a1d801
describe
'63467' 'info:fdaE20080623_AAAACEfileF20080623_AAAQLA' 'sip-files00042.QC.jpg'
1033a9bc4f22a45a9c022d86db218cc8
516e4d0824990b4bc141e9cbd7c4f449d1c24847
describe
'925524' 'info:fdaE20080623_AAAACEfileF20080623_AAAQLB' 'sip-files00042.tif'
5e422ae103fac36dd73dddf63d6a328d
4ad144e62dd88105bc9490a2cee2992824a58d52
describe
'3293' 'info:fdaE20080623_AAAACEfileF20080623_AAAQLC' 'sip-files00042.txt'
021b157b30a1dc030a85fb4227981038
7fac59075d4ce73edbe09398c14cf41ab7366625
describe
'15061' 'info:fdaE20080623_AAAACEfileF20080623_AAAQLD' 'sip-files00042thm.jpg'
466c55f18cf1f42b0d14c8add5fa4494
ecaed16d610a3336ab7c6eb1d0f6d17e7ba4aa15
describe
'32162' 'info:fdaE20080623_AAAACEfileF20080623_AAAQLE' 'sip-files00043.jp2'
fb075b507128c939a7f80ab014a20b8c
4a09e29159cd2c6c549db10df4c4c9a987cc33f7
describe
'37506' 'info:fdaE20080623_AAAACEfileF20080623_AAAQLF' 'sip-files00043.jpg'
ff8408172a12f7730aa3ba3b0247b656
b9124662faf1dd21d0492247194ac3c24010eb58
describe
'15185' 'info:fdaE20080623_AAAACEfileF20080623_AAAQLG' 'sip-files00043.pdf'
6272cfea9cf3ec4897465f5f1d50b7c2
3bd61817a650682e57845a183f1b96cb1ec7a84b
describe
'info:fdaE20080623_AAAACEfileF20080623_AAAQLG-norm-0' 'aip-filesF20080623_AAAQLG-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
'2017-03-09T11:27:55-05:00'
normalize
'10668' 'info:fdaE20080623_AAAACEfileF20080623_AAAQLH' 'sip-files00043.pro'
93853fa2bbb5d0ca7f4cf46666524ff6
e700bcc1b9e4ad56bdf05116ca84fb1d052baee6
describe
'11576' 'info:fdaE20080623_AAAACEfileF20080623_AAAQLI' 'sip-files00043.QC.jpg'
be678976beb2cd2f3894be8c2626b030
806a704e32d3a441e99abe05ed2918fc7b8ac718
describe
'898844' 'info:fdaE20080623_AAAACEfileF20080623_AAAQLJ' 'sip-files00043.tif'
1349edc150dd162f5573b0a24e2e44b9
8669346a2b8ac4d35c6478b98ed6dca58270fc43
describe
'406' 'info:fdaE20080623_AAAACEfileF20080623_AAAQLK' 'sip-files00043.txt'
f3d0f9154634341afd2d434e75b9dde9
be56ece7ef0367940469132dd5960d942212fa13
describe
'3468' 'info:fdaE20080623_AAAACEfileF20080623_AAAQLL' 'sip-files00043thm.jpg'
45f7abe29ce1c5d21c3bbcb99ec57e11
50857ec4131d7af3b41c548a56054949224e383a
describe
'164688' 'info:fdaE20080623_AAAACEfileF20080623_AAAQLM' 'sip-files00044.jp2'
58cbbffba7391d4f78f9b76ad6290361
6cd39e2401792b2a6ebf31d385b618a16e234089
describe
'158453' 'info:fdaE20080623_AAAACEfileF20080623_AAAQLN' 'sip-files00044.jpg'
f46ec970ebd0cf94a6a53c3d98533f6b
ab4498ecd895a970cdac375d70a3771692e41b73
describe
'67574' 'info:fdaE20080623_AAAACEfileF20080623_AAAQLO' 'sip-files00044.pdf'
4753e39ffd3461a2628a0b522d049f7e
c92e9a06001faed4de9a437305b6a68a7cd0ac9f
describe
'info:fdaE20080623_AAAACEfileF20080623_AAAQLO-norm-0' 'aip-filesF20080623_AAAQLO-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
'2017-03-09T11:24:19-05:00'
normalize
'62205' 'info:fdaE20080623_AAAACEfileF20080623_AAAQLP' 'sip-files00044.pro'
759742782d4fb7956508970a2c523faf
7682bb70fc1cc898a2c5ab3bca6b254e4ee1b4a3
describe
'52885' 'info:fdaE20080623_AAAACEfileF20080623_AAAQLQ' 'sip-files00044.QC.jpg'
a05b68b9a2dce0c2c6d5f1cf61971738
c4d968d9bfc16cc4ad305fdbb2cad2d93552bd12
'2017-03-09T11:27:43-05:00'
describe
'924224' 'info:fdaE20080623_AAAACEfileF20080623_AAAQLR' 'sip-files00044.tif'
3bdd8a9ec6519c22fa2d306e34e66b3e
50d56525e31bffcd4f185b946f70e95a823f0083
'2017-03-09T11:26:08-05:00'
describe
'2319' 'info:fdaE20080623_AAAACEfileF20080623_AAAQLS' 'sip-files00044.txt'
94e51023da3530175e31604b89b3dd4c
6c2db585751fce3ccd97d121fc60d97f12744327
describe
'13343' 'info:fdaE20080623_AAAACEfileF20080623_AAAQLT' 'sip-files00044thm.jpg'
9c3698383100eb3ad4943282a7767855
4b211c7735975b1d3b3e413d956eb6a42937f96d
describe
'56358' 'info:fdaE20080623_AAAACEfileF20080623_AAAQLU' 'sip-files00045.jp2'
86506cda4e3f8067af9ec16483b264d1
7d899d3c3087401eaa3e9a52315d9db4e1e5bc26
'2017-03-09T11:25:52-05:00'
describe
'58216' 'info:fdaE20080623_AAAACEfileF20080623_AAAQLV' 'sip-files00045.jpg'
21b76bc1dbc3520c2de615f8578abe73
1f0c9eccc89f96d9266f8c21b854441d55aeeda4
'2017-03-09T11:27:49-05:00'
describe
'24471' 'info:fdaE20080623_AAAACEfileF20080623_AAAQLW' 'sip-files00045.pdf'
e9bdbfd0ee5a786182ce3c97f0bbb9dd
b10c03e4b74f63ef1b568604a33c0e5960fee524
'2017-03-09T11:29:00-05:00'
describe
'info:fdaE20080623_AAAACEfileF20080623_AAAQLW-norm-0' 'aip-filesF20080623_AAAQLW-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
normalize
'20598' 'info:fdaE20080623_AAAACEfileF20080623_AAAQLX' 'sip-files00045.pro'
7e0348a3539a98982c645ebecad65e32
0b5c1970e5e80d49a4ea85bb839a28df4d783465
describe
'19033' 'info:fdaE20080623_AAAACEfileF20080623_AAAQLY' 'sip-files00045.QC.jpg'
f129a980a0f008cf80f4e740de41f61a
9e40580d5cbec49f87ec8b3ba66e3f2ce19d99ef
describe
'902416' 'info:fdaE20080623_AAAACEfileF20080623_AAAQLZ' 'sip-files00045.tif'
14e0f8cdc3a59a6576931c5dede0815a
66daa496372702d41ca471d65cd468421442c9a5
describe
'774' 'info:fdaE20080623_AAAACEfileF20080623_AAAQMA' 'sip-files00045.txt'
1c7bd883eef70372ad31cd9f51ad3c35
0fec00106b3793cf69addc44d86d4600e2fef790
describe
'5440' 'info:fdaE20080623_AAAACEfileF20080623_AAAQMB' 'sip-files00045thm.jpg'
a2a3ab0879614a16e6dfc90e60cf6427
853229024843e80dafc5951d9a575f3cabae36a7
describe
'169877' 'info:fdaE20080623_AAAACEfileF20080623_AAAQMC' 'sip-files00046.jp2'
1aecace286d55e934f0afd7934038a06
11c80c40e309c48cdc62a62b0edf13b0e1199d70
describe
'173178' 'info:fdaE20080623_AAAACEfileF20080623_AAAQMD' 'sip-files00046.jpg'
5bc43048a791dc2e2c30aa76c6755243
60f55e4b5f53f34259e005920a96a9a4cc16e3a1
describe
'68060' 'info:fdaE20080623_AAAACEfileF20080623_AAAQME' 'sip-files00046.pdf'
8c86f118c385c86fcac5a86816f80506
229e86ccfd56e48314d431e6a04a10db46942267
'2017-03-09T11:25:47-05:00'
describe
'info:fdaE20080623_AAAACEfileF20080623_AAAQME-norm-0' 'aip-filesF20080623_AAAQME-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
'2017-03-09T11:25:48-05:00'
normalize
'108541' 'info:fdaE20080623_AAAACEfileF20080623_AAAQMF' 'sip-files00046.pro'
f15851738e026634a2932db9059ff264
7c4a15f2dc86361576aceb0e2559ade1e2d1d0f0
describe
'57362' 'info:fdaE20080623_AAAACEfileF20080623_AAAQMG' 'sip-files00046.QC.jpg'
bb2c8de4b33a2106367699a44e245760
0d4b73b8438828067480f5f841455be98c6fb176
describe
'944508' 'info:fdaE20080623_AAAACEfileF20080623_AAAQMH' 'sip-files00046.tif'
d46722085d25dc190b974e58500513e8
e83f0f85d235059e8e7e07583b03191b90053765
describe
'4003' 'info:fdaE20080623_AAAACEfileF20080623_AAAQMI' 'sip-files00046.txt'
31ed6facc5819d4faeac92752acdbb32
2e17257c56ab23baff043b61741c988c5cd24f98
describe
'13517' 'info:fdaE20080623_AAAACEfileF20080623_AAAQMJ' 'sip-files00046thm.jpg'
35a4ca0bddce45bb24b0469bc91318a3
f19f64e43d9d0e4a35036d9ce7d84653a567158d
describe
'28048' 'info:fdaE20080623_AAAACEfileF20080623_AAAQMK' 'sip-files00047.jp2'
f72b17a2f5a4477f6478de419414cf99
a2cda01b0781fd5816d3d4f0d10d2877902238a1
describe
'33283' 'info:fdaE20080623_AAAACEfileF20080623_AAAQML' 'sip-files00047.jpg'
70c9b539d1c96e3ab8ea5e5e6be534ed
c7c54ba2db33158971053864ea148a2c56c8f857
describe
'12879' 'info:fdaE20080623_AAAACEfileF20080623_AAAQMM' 'sip-files00047.pdf'
f1022bf6abd6839633e870e71c0eb989
f3cfacf155dda7c22612f7c2fb1d207d85bbe5ee
'2017-03-09T11:28:56-05:00'
describe
'info:fdaE20080623_AAAACEfileF20080623_AAAQMM-norm-0' 'aip-filesF20080623_AAAQMM-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
'2017-03-09T11:28:58-05:00'
normalize
'12926' 'info:fdaE20080623_AAAACEfileF20080623_AAAQMN' 'sip-files00047.pro'
8d2255919ce5693a1c293ec2e0abd808
cf29876e0870924862221171b8621bcd8fc3095a
describe
'11175' 'info:fdaE20080623_AAAACEfileF20080623_AAAQMO' 'sip-files00047.QC.jpg'
fa3815772258d9c589356eb9e3db5623
97a14778fb4532ab83529322e10f3ad02580eb90
describe
'900840' 'info:fdaE20080623_AAAACEfileF20080623_AAAQMP' 'sip-files00047.tif'
c768a3f359d9402bba8b1acbbfbbcaab
7daf22cbfb634417c6be885723431353fe2c4695
describe
'503' 'info:fdaE20080623_AAAACEfileF20080623_AAAQMQ' 'sip-files00047.txt'
cc357965183011b375dfeac6a9ee7e13
4f9d78bec6001037e8ced9d10be88d283f76f22c
'2017-03-09T11:27:27-05:00'
describe
'3447' 'info:fdaE20080623_AAAACEfileF20080623_AAAQMR' 'sip-files00047thm.jpg'
e367b0fadf053b14bce135a37ead7056
12d6e6276c7638ae553ef36311f5eeaebd45765f
describe
'107275' 'info:fdaE20080623_AAAACEfileF20080623_AAAQMS' 'sip-files00048.jp2'
7a31ca7cea5ca9f7312146dff4b2351f
48e43d7366c98d22cd78deab76418a32d830bfb7
describe
'106475' 'info:fdaE20080623_AAAACEfileF20080623_AAAQMT' 'sip-files00048.jpg'
f62b6745ba46fc41895acd71538db1c0
c4f7562c029ffcd1643e75810aefa4d785888af0
describe
'41327' 'info:fdaE20080623_AAAACEfileF20080623_AAAQMU' 'sip-files00048.pdf'
977660849d9abef4dcd7b4453224b11a
6e69291f0b07d203b645054a4ef4c59a1607ed65
'2017-03-09T11:29:05-05:00'
describe
'info:fdaE20080623_AAAACEfileF20080623_AAAQMU-norm-0' 'aip-filesF20080623_AAAQMU-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
normalize
'89001' 'info:fdaE20080623_AAAACEfileF20080623_AAAQMV' 'sip-files00048.pro'
a93b59763b7b99894f8a9c0eeca3d951
60da5b13ef7ad8c7eea9657af90bf15f2bf1ddeb
describe
'36972' 'info:fdaE20080623_AAAACEfileF20080623_AAAQMW' 'sip-files00048.QC.jpg'
962a4854391cf844427c39b1a78f68c3
44acbba1927807bef26a72b5e765e20960e7f25f
describe
'940160' 'info:fdaE20080623_AAAACEfileF20080623_AAAQMX' 'sip-files00048.tif'
baaeac7931a62999aba301ff3044866a
444fce3b8dd106cc3cafd93d82054df0dcf546ec
describe
'2884' 'info:fdaE20080623_AAAACEfileF20080623_AAAQMY' 'sip-files00048.txt'
27db9cc0c9ee36b95fa995f9302114a4
684d4dcb3385f26fb952bd2e5e0df1a6d1d57763
describe
'9889' 'info:fdaE20080623_AAAACEfileF20080623_AAAQMZ' 'sip-files00048thm.jpg'
b031e5211ba2712d070e31557a402fc6
2b343951a9852fa47c401079b70bb609fbb6d889
describe
'98826' 'info:fdaE20080623_AAAACEfileF20080623_AAAQNA' 'sip-files00049.jp2'
4d63c626c6711863271df5e85764e542
99bb47d40a945c72e6bd09a89aecd4ea3b035683
'2017-03-09T11:27:07-05:00'
describe
'100559' 'info:fdaE20080623_AAAACEfileF20080623_AAAQNB' 'sip-files00049.jpg'
b9c073b7d4a70223c5cba76eb88157b7
e7ba542bfdda1b3ec885d0b087eb305d16085b7f
describe
'37818' 'info:fdaE20080623_AAAACEfileF20080623_AAAQNC' 'sip-files00049.pdf'
9b4ef0c2a560550de0e5f493b2154c1a
090005b608d42f8beba1204f44031adb239f1f45
describe
'info:fdaE20080623_AAAACEfileF20080623_AAAQNC-norm-0' 'aip-filesF20080623_AAAQNC-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
normalize
'86666' 'info:fdaE20080623_AAAACEfileF20080623_AAAQND' 'sip-files00049.pro'
21920178d8b77399b65dc08bc9484e62
2ffb1bd2e3154acc03bd5defdf71a1dbfb441f09
describe
'33918' 'info:fdaE20080623_AAAACEfileF20080623_AAAQNE' 'sip-files00049.QC.jpg'
3250989774d1816b54da82366931263a
a31d2b5aaf6ee2b3af8a8845f5762edf87029868
'2017-03-09T11:27:56-05:00'
describe
'905580' 'info:fdaE20080623_AAAACEfileF20080623_AAAQNF' 'sip-files00049.tif'
61e242fd39b08e0056b88659ba6cbc80
49ddfce409a0f21bfd3e59e27f3489ded72ba2e7
describe
'2595' 'info:fdaE20080623_AAAACEfileF20080623_AAAQNG' 'sip-files00049.txt'
e1d6a8e9813844bbcd67691da4a41c0c
c502adb21bd16fec3b0c136a04209fefb093ad55
describe
'9600' 'info:fdaE20080623_AAAACEfileF20080623_AAAQNH' 'sip-files00049thm.jpg'
45a35595299c1d0488f90f8cdf94891c
411fee4bbc3d12bc7a90bafd47186272aba8c2f2
describe
'112526' 'info:fdaE20080623_AAAACEfileF20080623_AAAQNI' 'sip-files00050.jp2'
0ae292caf9a26a3bf52c63423dd1bcf6
1d2e49fbe7aadc79ae138a0a3be697a59fbbafe5
describe
'112443' 'info:fdaE20080623_AAAACEfileF20080623_AAAQNJ' 'sip-files00050.jpg'
89f56e08a718bbbb7083821bbf1d904e
8725de46b6df26e970e399260366625f353952f9
describe
'43539' 'info:fdaE20080623_AAAACEfileF20080623_AAAQNK' 'sip-files00050.pdf'
196895874cc9de70a51df18dc82c2f72
4d863dab9eb6a3b46acd71e85e2b15400f3d48ba
'2017-03-09T11:26:19-05:00'
describe
'info:fdaE20080623_AAAACEfileF20080623_AAAQNK-norm-0' 'aip-filesF20080623_AAAQNK-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
'2017-03-09T11:26:20-05:00'
normalize
'82425' 'info:fdaE20080623_AAAACEfileF20080623_AAAQNL' 'sip-files00050.pro'
590ae241e40601a39b74fdae84d73e7e
a593b3c0ebafcc983b098ed75c2bb09b8bb5a26a
describe
'38035' 'info:fdaE20080623_AAAACEfileF20080623_AAAQNM' 'sip-files00050.QC.jpg'
39ccae0da9f6e157c137b7513e82e5f2
05a5ec00373cd79f97f3207e1fc232f276a364dc
describe
'939784' 'info:fdaE20080623_AAAACEfileF20080623_AAAQNN' 'sip-files00050.tif'
c09ac88d64efc745a567bee3bf00e21a
964c1be1ff7d28ee7071eafeaf8397a568ecf7da
describe
'3462' 'info:fdaE20080623_AAAACEfileF20080623_AAAQNO' 'sip-files00050.txt'
7f923b65020b50d34721c2cd94c6a7c6
1132bffb4c8f6d7119b5cb3680a4906e63429816
describe
'9194' 'info:fdaE20080623_AAAACEfileF20080623_AAAQNP' 'sip-files00050thm.jpg'
0860872b16d89a6bcdb4938b4d6234fb
21e03e94ce7884ff13584bf7df54b5f6bfdfbb79
describe
'111142' 'info:fdaE20080623_AAAACEfileF20080623_AAAQNQ' 'sip-files00051.jp2'
f465525e99b452a6665b446a73cec72e
5dbb24733bc85ca16d07ddb87526bab65875a259
describe
'117148' 'info:fdaE20080623_AAAACEfileF20080623_AAAQNR' 'sip-files00051.jpg'
3160e6cfcc63fd951f67d21d45edd56f
4cad38eb1a39b7d0256877d4ede88b2d837eeb53
'2017-03-09T11:24:20-05:00'
describe
'43700' 'info:fdaE20080623_AAAACEfileF20080623_AAAQNS' 'sip-files00051.pdf'
4427cda49a172d85356de81a70839bb0
ae1927d5012c7335c5d43d8a92cd673d9eaa03fb
describe
'info:fdaE20080623_AAAACEfileF20080623_AAAQNS-norm-0' 'aip-filesF20080623_AAAQNS-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
normalize
'74857' 'info:fdaE20080623_AAAACEfileF20080623_AAAQNT' 'sip-files00051.pro'
747fd9476c282429555be734cbbc79c3
976bf8600e738ecd2791068b59ef77297023bde9
describe
'39589' 'info:fdaE20080623_AAAACEfileF20080623_AAAQNU' 'sip-files00051.QC.jpg'
18d48244076d61ee285fff65c8d36da1
5448e0c741ae2e242775362733f285add18226db
describe
'905844' 'info:fdaE20080623_AAAACEfileF20080623_AAAQNV' 'sip-files00051.tif'
be89a7e3981040c52a61d36218f153a0
7981cb891e5a44ea1ccc094b8ac0e361fc850be1
'2017-03-09T11:28:35-05:00'
describe
'2702' 'info:fdaE20080623_AAAACEfileF20080623_AAAQNW' 'sip-files00051.txt'
459761f6694e8823eb8a416a41c803f6
70304e557a7ea6228c4c69a834139b5331d33f5c
describe
'9796' 'info:fdaE20080623_AAAACEfileF20080623_AAAQNX' 'sip-files00051thm.jpg'
c018422c830fd7f62104e88179301d3e
468e6e0f2404e9df1c57d6d1ad3d4554db662260
describe
'107476' 'info:fdaE20080623_AAAACEfileF20080623_AAAQNY' 'sip-files00052.jp2'
81759afb2067ecf36f14488dfdb5ad31
d16ecac9e7ea3d0ab6e095ed6d1909677fb9cdc7
describe
'108090' 'info:fdaE20080623_AAAACEfileF20080623_AAAQNZ' 'sip-files00052.jpg'
c4987530ebf2ad439e51ad0294caf2cb
687e0be61aac4c55e8447032be3057aff3007eb0
describe
'41473' 'info:fdaE20080623_AAAACEfileF20080623_AAAQOA' 'sip-files00052.pdf'
ff92969fe564d1f59932a39bd272b8ab
9119249d3874e9bedf185d12265546d750a78d10
describe
'info:fdaE20080623_AAAACEfileF20080623_AAAQOA-norm-0' 'aip-filesF20080623_AAAQOA-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
'2017-03-09T11:24:49-05:00'
normalize
'63017' 'info:fdaE20080623_AAAACEfileF20080623_AAAQOB' 'sip-files00052.pro'
667c15f7c8d09735b01b1b58d745c185
a92468d3ce9d8fc4b698b347d30fe433be586883
describe
'36202' 'info:fdaE20080623_AAAACEfileF20080623_AAAQOC' 'sip-files00052.QC.jpg'
3173396509a550eb1f4794bfcc369942
c24dd2e6c6695027d821a733a4c65c4dce3333bf
describe
'927700' 'info:fdaE20080623_AAAACEfileF20080623_AAAQOD' 'sip-files00052.tif'
1b212adf794e94cae68b71ddcd54a051
429f46867723ddc8fe974c640f58ca242e47c99e
'2017-03-09T11:28:07-05:00'
describe
'2363' 'info:fdaE20080623_AAAACEfileF20080623_AAAQOE' 'sip-files00052.txt'
83ba6b5185a4ed56b6e2675f540d6cb8
423deac83bfc465a9148d4037191ee32a65bf0cb
describe
'9692' 'info:fdaE20080623_AAAACEfileF20080623_AAAQOF' 'sip-files00052thm.jpg'
60161fe2c950338238f1d9f4d0948f68
19d27cf1841df5fa4e1a15f89aca584f0c785bb4
describe
'31170' 'info:fdaE20080623_AAAACEfileF20080623_AAAQOG' 'sip-files00053.jp2'
f655c12b72274105677570b872a6b6d5
6feba4d9eb29b190b1b41556b840c3a68d246d70
describe
'36538' 'info:fdaE20080623_AAAACEfileF20080623_AAAQOH' 'sip-files00053.jpg'
f801f7e393364affd748dcae0e05f6c0
fe14026c77f9f95231278528feb1d590a5f6fa9d
describe
'13447' 'info:fdaE20080623_AAAACEfileF20080623_AAAQOI' 'sip-files00053.pdf'
d44f4eb438e9f15c2a5bd2fbd1321431
88e924b4ea4f9dc2b4dde62b1475b02ae0ad4ea2
describe
'info:fdaE20080623_AAAACEfileF20080623_AAAQOI-norm-0' 'aip-filesF20080623_AAAQOI-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
'2017-03-09T11:25:14-05:00'
normalize
'17074' 'info:fdaE20080623_AAAACEfileF20080623_AAAQOJ' 'sip-files00053.pro'
bf025b9c6e08f24e706027a08fe0b67b
3a2b72da71357c81f31188d861d84c67ee876142
describe
'12609' 'info:fdaE20080623_AAAACEfileF20080623_AAAQOK' 'sip-files00053.QC.jpg'
8a0870dc73f0671ec1208cb4f9875b64
a9bb953737552b4fa4c621c6f844b5a397d7eb61
describe
'880500' 'info:fdaE20080623_AAAACEfileF20080623_AAAQOL' 'sip-files00053.tif'
c2d0920e0666d06605839fdfb914d481
5f7aef2414b092335bb6e995b445d3c0de45a5d0
describe
'618' 'info:fdaE20080623_AAAACEfileF20080623_AAAQOM' 'sip-files00053.txt'
9a686c08c32036e389d2bbde487888ca
1461a6627cb79216bd35ef49caaefc67cdbe53ba
describe
'3786' 'info:fdaE20080623_AAAACEfileF20080623_AAAQON' 'sip-files00053thm.jpg'
ea57b68fa510ec268684c1dec0557f36
88fa62de044e603e70d29c61b5da83de4f008cbb
'2017-03-09T11:28:10-05:00'
describe
'17812' 'info:fdaE20080623_AAAACEfileF20080623_AAAQOO' 'sip-files00054.jp2'
bb13145d63475dc93e34e2383a5ab3f0
5ae1bbb921f519d94733381ed4f8832c23e8b9c3
'2017-03-09T11:27:11-05:00'
describe
'22763' 'info:fdaE20080623_AAAACEfileF20080623_AAAQOP' 'sip-files00054.jpg'
d4764786274993e812c6a0f8c0d51f8d
259a0bcf228fe1644a31f9e00cab7c137cc1eb44
describe
'8123' 'info:fdaE20080623_AAAACEfileF20080623_AAAQOQ' 'sip-files00054.pdf'
8c72a8c979e30fece9d8d71ac2234d54
dc68e6c68555a13268cf2ec9467f702db3b7a84f
describe
'info:fdaE20080623_AAAACEfileF20080623_AAAQOQ-norm-0' 'aip-filesF20080623_AAAQOQ-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
normalize
'3880' 'info:fdaE20080623_AAAACEfileF20080623_AAAQOR' 'sip-files00054.pro'
62833ef9bd26aa830e833c4be2a8bedd
a2d9bca844e4c9fa92d2b5793b5e22e8697f7a15
describe
'7929' 'info:fdaE20080623_AAAACEfileF20080623_AAAQOS' 'sip-files00054.QC.jpg'
5d7f72bc28d55cdb6fd69d286882a730
6ef90064c54f946fdd4edda551f92d03cef1ea50
describe
'899844' 'info:fdaE20080623_AAAACEfileF20080623_AAAQOT' 'sip-files00054.tif'
aa5e5a9edfb1004b0a63167e4364b102
ce6543426571da309885fca78354cd45e689ad71
describe
'190' 'info:fdaE20080623_AAAACEfileF20080623_AAAQOU' 'sip-files00054.txt'
7a5c4af4f0436b25399c0ac6f9933404
50d8851fb4edbd082a94ae8fd8c7425fda8c0f00
describe
'2707' 'info:fdaE20080623_AAAACEfileF20080623_AAAQOV' 'sip-files00054thm.jpg'
a4799e6e8125aa8d8ebd84a9e9454635
e9d1630e22a56dc98770b1a735ab73cf1ffed152
describe
'info:fdaE20080623_AAAACEfileF20080623_AAAQOW' 'sip-files00055.jp2'
236e7d719199c154f784e5196a33e70b
5ecf596e8f9bdcec5722058f76321640d0674eed
describe
'45141' 'info:fdaE20080623_AAAACEfileF20080623_AAAQOX' 'sip-files00055.jpg'
4de926f0179fa1a04ed3a183e2ecd947
800418d4c14d7fb55471b8b493c5461c3c3d5ec9
describe
'39754' 'info:fdaE20080623_AAAACEfileF20080623_AAAQOY' 'sip-files00055.pdf'
5a2f336a5fdb5877c8965fdc73bd6334
1996876ab6997c2734bd2c5b9185867c795d1866
describe
'info:fdaE20080623_AAAACEfileF20080623_AAAQOY-norm-0' 'aip-filesF20080623_AAAQOY-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
normalize
'54866' 'info:fdaE20080623_AAAACEfileF20080623_AAAQOZ' 'sip-files00055.pro'
e667a0b6fa05af7cf5c23103e86699cd
3aa1312a8a79ab4a3ee8b55207eaad6dc2b29f13
describe
'16974' 'info:fdaE20080623_AAAACEfileF20080623_AAAQPA' 'sip-files00055.QC.jpg'
a8de1fe0ea43d5d9f09b1f0f65eb2dab
053b96b4a21d5371a9eeb889b0bdd0b47eeea311
describe
'932856' 'info:fdaE20080623_AAAACEfileF20080623_AAAQPB' 'sip-files00055.tif'
ece4621982a6e06b96cf95f493eb1cbc
031939dc70c4d273cc450cc331f33941aa47952f
'2017-03-09T11:27:40-05:00'
describe
'2950' 'info:fdaE20080623_AAAACEfileF20080623_AAAQPC' 'sip-files00055.txt'
131abfe63ec14d1f53eb3289a0610cca
67c7594613aca8fbe1872201c6d4fb618b14e45f
describe
'5313' 'info:fdaE20080623_AAAACEfileF20080623_AAAQPD' 'sip-files00055thm.jpg'
cb1a5a5518e30765a0a5fa478a0803da
2d548d2d41063bf7181b6f6a11e600badcdd3c12
describe
'106018' 'info:fdaE20080623_AAAACEfileF20080623_AAAQPE' 'sip-files00056.jp2'
a40c3d43f3e6e20eb7b619a834df15da
04739b11f2025655fd1c71e12146e23bb09dae51
describe
'49170' 'info:fdaE20080623_AAAACEfileF20080623_AAAQPF' 'sip-files00056.jpg'
1759e67e4eeb7db351d30cb6055f00c2
5cb89ffb9de3ccc6373d2b4ea5d9e9f1bfe3cf21
describe
'44196' 'info:fdaE20080623_AAAACEfileF20080623_AAAQPG' 'sip-files00056.pdf'
cb77ada90bc56f05cfbe9725aabde2e7
7c6eebb0292354646458e31c06b001d6132b0636
describe
'info:fdaE20080623_AAAACEfileF20080623_AAAQPG-norm-0' 'aip-filesF20080623_AAAQPG-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
normalize
'60977' 'info:fdaE20080623_AAAACEfileF20080623_AAAQPH' 'sip-files00056.pro'
e6adec3dd71e6b57f124636ee38d7819
19b1f136951d288d4522a669e187b71ff2bb8db1
'2017-03-09T11:25:05-05:00'
describe
'17223' 'info:fdaE20080623_AAAACEfileF20080623_AAAQPI' 'sip-files00056.QC.jpg'
62e31a64b39cdcf8be1e3dc89af89de6
05ad687a971edd94ddf614f68edb2ec3129f6719
describe
'913300' 'info:fdaE20080623_AAAACEfileF20080623_AAAQPJ' 'sip-files00056.tif'
5536dc87bd70ea8229e80bbdb408c130
1a47eebd35df94d9158011b09915d7ffe135ec46
describe
'3287' 'info:fdaE20080623_AAAACEfileF20080623_AAAQPK' 'sip-files00056.txt'
b091d599eb14e248590aa2436173543e
098b4969b6a8f8138ecf570de5ca45744bd856d5
describe
Invalid character
Invalid character
'5377' 'info:fdaE20080623_AAAACEfileF20080623_AAAQPL' 'sip-files00056thm.jpg'
80a29b22b10d48a334c4b3ba40de54dc
3ac7d5245a94e8ca2ffe354adfd16d97dc57e3ea
describe
'98566' 'info:fdaE20080623_AAAACEfileF20080623_AAAQPM' 'sip-files00057.jp2'
ba0fcb37b1dd0f269b7a3a67f5edf719
001d78408310807e1ae0c3e92cebafe692364398
describe
'42951' 'info:fdaE20080623_AAAACEfileF20080623_AAAQPN' 'sip-files00057.jpg'
20d7c366636b27eef24ba0a2dce90d79
e2cd0cda8822a8d75442e3b9b4c18f02b49530cc
describe
'41214' 'info:fdaE20080623_AAAACEfileF20080623_AAAQPO' 'sip-files00057.pdf'
44db57b4fdb5db5f2639af18d151e394
7036fac0f5421bc154157f24df03778456b734c9
describe
'info:fdaE20080623_AAAACEfileF20080623_AAAQPO-norm-0' 'aip-filesF20080623_AAAQPO-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
normalize
'60728' 'info:fdaE20080623_AAAACEfileF20080623_AAAQPP' 'sip-files00057.pro'
ed0f4244b297f4c9c17d45b734f34853
d6fb54d4918ff3e89fad6833e8d8685d215d07dd
describe
'15048' 'info:fdaE20080623_AAAACEfileF20080623_AAAQPQ' 'sip-files00057.QC.jpg'
680364e5933a20336d38758477323a3e
2687ecb5fc4fb527a323fd74609332719c2c284e
describe
'939820' 'info:fdaE20080623_AAAACEfileF20080623_AAAQPR' 'sip-files00057.tif'
9bf57493d79fd5940d64e8aba289b8cd
ede996002dda1f2ee057e06371a134014046d140
describe
'3324' 'info:fdaE20080623_AAAACEfileF20080623_AAAQPS' 'sip-files00057.txt'
0a24f8c241d816c387cf8160ff2512b4
8b3d06ceea71020732211401feac7702b12fcd52
describe
'5150' 'info:fdaE20080623_AAAACEfileF20080623_AAAQPT' 'sip-files00057thm.jpg'
b029c1cf97fe9e206dcca8deb00592db
b52a7a7b4a8eb94b8e8f7e27e05e2ca3f08977b7
describe
'83921' 'info:fdaE20080623_AAAACEfileF20080623_AAAQPU' 'sip-files00058.jp2'
9450cbd224f69f58e6877d37f963a97f
d7b7a611a84e14daa322b3e4aaa0b3923d27c130
describe
'36533' 'info:fdaE20080623_AAAACEfileF20080623_AAAQPV' 'sip-files00058.jpg'
2b516f2689e818ccc3f8c16b72d7227f
bfc063bdad6ccd95ec9dbadbc37b6381208b51e0
describe
'34736' 'info:fdaE20080623_AAAACEfileF20080623_AAAQPW' 'sip-files00058.pdf'
678d8db2d995e6d2ef0d529ab409d02e
75420a9697ee651c06bb553965a7a981444f2b48
describe
'info:fdaE20080623_AAAACEfileF20080623_AAAQPW-norm-0' 'aip-filesF20080623_AAAQPW-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
'2017-03-09T11:27:01-05:00'
normalize
'47713' 'info:fdaE20080623_AAAACEfileF20080623_AAAQPX' 'sip-files00058.pro'
54971392e7f25608ab30d669a6e16fda
6c1c49c1d357bb20cfea7a60be3a1075978678e5
describe
'13618' 'info:fdaE20080623_AAAACEfileF20080623_AAAQPY' 'sip-files00058.QC.jpg'
2c10e5ea2f270db5e17fbe6320f4676e
11b02574cb6c22d7235344ed24e735cb09feaf23
describe
'929084' 'info:fdaE20080623_AAAACEfileF20080623_AAAQPZ' 'sip-files00058.tif'
7fb036a945b78d9cfdb3bbc299126044
bfe96acbb5f34ec39423929f669abb96a8169edc
describe
'2536' 'info:fdaE20080623_AAAACEfileF20080623_AAAQQA' 'sip-files00058.txt'
6c23b2177b102ce40d210935213a6260
7e3904faff939d4e275e112a97ea95c1063d79a4
describe
'4577' 'info:fdaE20080623_AAAACEfileF20080623_AAAQQB' 'sip-files00058thm.jpg'
46d33b49aa9d0ec5737d52ec5cf4f973
9c0cc1762b4111098178aabe8d13cec8678e239e
describe
'99788' 'info:fdaE20080623_AAAACEfileF20080623_AAAQQC' 'sip-files00059.jp2'
2654f1c345266da8b70168992a103971
3a9db709185d5c77ff77cdde4758bff4cdb202a3
describe
'46506' 'info:fdaE20080623_AAAACEfileF20080623_AAAQQD' 'sip-files00059.jpg'
3177f55b30ab663f84af2d6374298533
79b28a454b32c92f430f7c3b1655fc856bac7a03
describe
'41708' 'info:fdaE20080623_AAAACEfileF20080623_AAAQQE' 'sip-files00059.pdf'
6428136ffc38417e4e49964593d0c1bc
13bcbc7e3f42118104f434d10f3253331ff04ead
describe
'info:fdaE20080623_AAAACEfileF20080623_AAAQQE-norm-0' 'aip-filesF20080623_AAAQQE-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
normalize
'63271' 'info:fdaE20080623_AAAACEfileF20080623_AAAQQF' 'sip-files00059.pro'
19c54f59160d7948fb255cde2f50b720
fb95c97e170401e8c01aeec2fc91d0b6787f63dd
describe
'15863' 'info:fdaE20080623_AAAACEfileF20080623_AAAQQG' 'sip-files00059.QC.jpg'
d99acebb259dd98e1eff71de47b50c23
c4bd1d73fd01f5c8b804a1ca57c4f03b25f20af8
describe
'936512' 'info:fdaE20080623_AAAACEfileF20080623_AAAQQH' 'sip-files00059.tif'
0b0d52bb5bb32fbbdb5f1942a0488684
7f0304daa17445d5493b2efb9b9fe51096d423bd
describe
'3697' 'info:fdaE20080623_AAAACEfileF20080623_AAAQQI' 'sip-files00059.txt'
dd6140b1f59404bdd9db1f915fd6db44
5e3579d476b0c8e5f45d5745b54cef43568af741
describe
'5009' 'info:fdaE20080623_AAAACEfileF20080623_AAAQQJ' 'sip-files00059thm.jpg'
9133857ed10dfac403b93c3fa9322e06
75883de694e56f8d7efa19ab58df7b5868825533
describe
'91632' 'info:fdaE20080623_AAAACEfileF20080623_AAAQQK' 'sip-files00060.jp2'
22053430327dd9c6cb4974f3e5a33d6a
e23fb7a8e6c275906eb49ca70269c5fe65f2a7f2
describe
'39489' 'info:fdaE20080623_AAAACEfileF20080623_AAAQQL' 'sip-files00060.jpg'
442f40cca7965fb5e5afd6c3b87224ca
1a90d3a4db5a16556fe7b00eedfed9899ec66665
describe
'38825' 'info:fdaE20080623_AAAACEfileF20080623_AAAQQM' 'sip-files00060.pdf'
74115f642e0b1aeee7019f86357f23e0
a62fc2c731dc6b94c1313f04eb837bbe9e9a40cd
'2017-03-09T11:26:11-05:00'
describe
'info:fdaE20080623_AAAACEfileF20080623_AAAQQM-norm-0' 'aip-filesF20080623_AAAQQM-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
normalize
'51724' 'info:fdaE20080623_AAAACEfileF20080623_AAAQQN' 'sip-files00060.pro'
9e717f2bf3596f8c81ca1ff9c2ad3a6f
1798bfd548fb7c249b878718e3ce938fa81a21a9
describe
'13370' 'info:fdaE20080623_AAAACEfileF20080623_AAAQQO' 'sip-files00060.QC.jpg'
28299771cc0a7fa8577aa090ff0685e9
6d65b50586d2a0c9bcaf85836a62c045b38a1e50
describe
'929000' 'info:fdaE20080623_AAAACEfileF20080623_AAAQQP' 'sip-files00060.tif'
f44defbde2f3d80c88bbb3ec15a7fe54
1148431fa7eabb03a01b9b1ddd8de94ffb226c0a
describe
'2914' 'info:fdaE20080623_AAAACEfileF20080623_AAAQQQ' 'sip-files00060.txt'
79fdd6cb5ff8012b9be33d601bb20a32
52ebbc0bbced9bc55c691ce17657dcc17bda519f
describe
Invalid character
Invalid character
'4810' 'info:fdaE20080623_AAAACEfileF20080623_AAAQQR' 'sip-files00060thm.jpg'
4dcb32c62bbd742a1b13a20466b18d52
64b3004a4cc15c69648bb59408cf2a801792af59
'2017-03-09T11:27:25-05:00'
describe
'89569' 'info:fdaE20080623_AAAACEfileF20080623_AAAQQS' 'sip-files00061.jp2'
4d8209838c8e804cd0b7009409c10618
b7459bd2d966649215cf37a0577f419cd92ee952
describe
'38878' 'info:fdaE20080623_AAAACEfileF20080623_AAAQQT' 'sip-files00061.jpg'
32d3685311715728b532b9a97dbb75ba
802dcd6342f535a198148a869bc5de5e84cf6fa9
describe
'37382' 'info:fdaE20080623_AAAACEfileF20080623_AAAQQU' 'sip-files00061.pdf'
c56f1332b872cf8c52a449f3d9562a9a
1902b278641c81645db68b3fda7289acbbe6c464
describe
'info:fdaE20080623_AAAACEfileF20080623_AAAQQU-norm-0' 'aip-filesF20080623_AAAQQU-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
normalize
'54419' 'info:fdaE20080623_AAAACEfileF20080623_AAAQQV' 'sip-files00061.pro'
7edac79db50832f4463ca18e269f22c1
c4c2468503c839339fe9b37f537d7d2328a8970d
describe
'14330' 'info:fdaE20080623_AAAACEfileF20080623_AAAQQW' 'sip-files00061.QC.jpg'
81aa1595c8f69485cad32fcd1116f90d
8d4596a59cf8cd009d1c5ab54f8184cc4401d027
describe
'920380' 'info:fdaE20080623_AAAACEfileF20080623_AAAQQX' 'sip-files00061.tif'
05e2fc658dd366cfbe4a17b31967b055
32566a88eef7b1f791d9ed14f9bc04bd6f583131
describe
'2892' 'info:fdaE20080623_AAAACEfileF20080623_AAAQQY' 'sip-files00061.txt'
2798bd2d9d3a9ced662a61f5c308bf95
c3a95d91133d3952d72a91b088d73bec14987ef6
describe
Invalid character
Invalid character
'4788' 'info:fdaE20080623_AAAACEfileF20080623_AAAQQZ' 'sip-files00061thm.jpg'
31d901051e09bd447ae390b8e3e05fba
44403c17a878578fd00c9fd88ca4d9fcd7cfd888
describe
'84643' 'info:fdaE20080623_AAAACEfileF20080623_AAAQRA' 'sip-files00062.jp2'
3eb466ee5fe66912c21bbdff68a4235b
476413854c6fa291f65634bd2cfdb371283e27d3
describe
'37189' 'info:fdaE20080623_AAAACEfileF20080623_AAAQRB' 'sip-files00062.jpg'
970a80e01a04ee5ec45713cf4f79aebd
de43404c28d3ee9204d4cc77c3ce19342705b82e
describe
'35477' 'info:fdaE20080623_AAAACEfileF20080623_AAAQRC' 'sip-files00062.pdf'
1549308f2b9b8e79d73096e4cbf2469c
4d7d1b6a9f44af99ce6c8044d741b07588794626
'2017-03-09T11:27:23-05:00'
describe
'info:fdaE20080623_AAAACEfileF20080623_AAAQRC-norm-0' 'aip-filesF20080623_AAAQRC-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
normalize
'48293' 'info:fdaE20080623_AAAACEfileF20080623_AAAQRD' 'sip-files00062.pro'
4c6a9504df590150564f35083850ae93
54550fa8546952dd49736737d431762b76990acf
describe
'13096' 'info:fdaE20080623_AAAACEfileF20080623_AAAQRE' 'sip-files00062.QC.jpg'
161c1b3edec2b1e2999f74d82ee54a30
0470ab9a129875f10a277106a28d9e58d9fe5c56
describe
'909600' 'info:fdaE20080623_AAAACEfileF20080623_AAAQRF' 'sip-files00062.tif'
53fab0c5c11ac70ccb5758877fcd7dfc
1ea91634b44b8cf0941ef14a1a1cc0c33e816bf8
describe
'2888' 'info:fdaE20080623_AAAACEfileF20080623_AAAQRG' 'sip-files00062.txt'
a4453fd6c33e1f8dc968299298acb2c3
daa56991ebfbd63065f6b2168e6f0e1c0e51e899
describe
'4616' 'info:fdaE20080623_AAAACEfileF20080623_AAAQRH' 'sip-files00062thm.jpg'
e28ada8682c46baba9b57e93d0a129db
f5d018167e86ce2ab7e06814612cdfb450a3d1df
describe
'76726' 'info:fdaE20080623_AAAACEfileF20080623_AAAQRI' 'sip-files00063.jp2'
ccade0bcffda680b579e489decde9d98
ada85bce4dd48d0608f572ef58fa950768643197
describe
'34977' 'info:fdaE20080623_AAAACEfileF20080623_AAAQRJ' 'sip-files00063.jpg'
5151890bc83a983668bcd6c7030d3859
a5457562b6dc8c2ae539e6fd0273b979feaa08ef
describe
'32568' 'info:fdaE20080623_AAAACEfileF20080623_AAAQRK' 'sip-files00063.pdf'
b01d0fb56065e086fb832f95a0b39951
78e2ab0795cde904cc2caf4e4cc936878a591ce7
describe
'info:fdaE20080623_AAAACEfileF20080623_AAAQRK-norm-0' 'aip-filesF20080623_AAAQRK-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
'2017-03-09T11:26:10-05:00'
normalize
'45829' 'info:fdaE20080623_AAAACEfileF20080623_AAAQRL' 'sip-files00063.pro'
f481ee787a9de05a8a2659c61879d933
e822d4a5bca00300edd3d886c20a569dd4a42d3a
describe
'12573' 'info:fdaE20080623_AAAACEfileF20080623_AAAQRM' 'sip-files00063.QC.jpg'
265d06d3b0b9088fb335d5f98f161f22
985d937ba797c6113d1c33142db18e67a9ed1d00
describe
'950416' 'info:fdaE20080623_AAAACEfileF20080623_AAAQRN' 'sip-files00063.tif'
82130f675ca19fd8f1b7a8805683bf2f
f0b57c0883710f3cc4a51a15dd1d1b538e7dec7e
describe
'2753' 'info:fdaE20080623_AAAACEfileF20080623_AAAQRO' 'sip-files00063.txt'
a52d39c75c512542b16a27d003eaaea2
7e73474480f6e54ab0217cfb52ac554530d59511
describe
'4271' 'info:fdaE20080623_AAAACEfileF20080623_AAAQRP' 'sip-files00063thm.jpg'
9175ba0002326df4a8e06c5539a2a3ef
d8692e5520b5619cce3f0c8133742539f94268c1
describe
'83410' 'info:fdaE20080623_AAAACEfileF20080623_AAAQRQ' 'sip-files00064.jp2'
64a28dd34b704d4069d842246ab00d57
08bca30dc3b9f5a676df74402c4398e2706f9334
'2017-03-09T11:25:19-05:00'
describe
'38190' 'info:fdaE20080623_AAAACEfileF20080623_AAAQRR' 'sip-files00064.jpg'
4267905ab18a123c842be619b713d3e6
b4654c76cab87c3b17e2dd473b7fa7b3e065252b
describe
'34558' 'info:fdaE20080623_AAAACEfileF20080623_AAAQRS' 'sip-files00064.pdf'
ddb17e7bfde62e4c36828e9773d1a67b
9dd3c9f8b1893e88a67fe80f5b37252ff7cc8df1
'2017-03-09T11:25:37-05:00'
describe
'info:fdaE20080623_AAAACEfileF20080623_AAAQRS-norm-0' 'aip-filesF20080623_AAAQRS-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
normalize
'45286' 'info:fdaE20080623_AAAACEfileF20080623_AAAQRT' 'sip-files00064.pro'
66af1ec11c39ce38438381c23af2fd92
887a9ea5d5c4429401995ab733492fa8becf58f2
describe
'13441' 'info:fdaE20080623_AAAACEfileF20080623_AAAQRU' 'sip-files00064.QC.jpg'
45b73396256a8c58c43271996e5ca0c0
58f48439d5f4e9a7cb3ef1b12b3a89497c493ab7
describe
'939192' 'info:fdaE20080623_AAAACEfileF20080623_AAAQRV' 'sip-files00064.tif'
01f34650c66b8cd459f5003dd34e6f57
90261fe02649dd411cee55b716723837d82b1e62
describe
'2405' 'info:fdaE20080623_AAAACEfileF20080623_AAAQRW' 'sip-files00064.txt'
e6fb8ba704e00384cea51c07ca40cbd5
9cbddca9ecf053ab72e442b45c30a9be366ea909
describe
'4635' 'info:fdaE20080623_AAAACEfileF20080623_AAAQRX' 'sip-files00064thm.jpg'
e75d5da80bede7297d1092cf5b957821
21735882b003277efda5aa71cc60df5cddeee00d
describe
'89877' 'info:fdaE20080623_AAAACEfileF20080623_AAAQRY' 'sip-files00065.jp2'
0400fc6ead2b4591bdd8d54c16c01c5a
37287272b47400a9a77fe866bd6b55d9655d200f
describe
'39343' 'info:fdaE20080623_AAAACEfileF20080623_AAAQRZ' 'sip-files00065.jpg'
cb277883d2269ff2513e22ae537a03ec
be34c7d5dff88238b1955910244148d257477f1d
describe
'37566' 'info:fdaE20080623_AAAACEfileF20080623_AAAQSA' 'sip-files00065.pdf'
cae17fcb6825bd5d130d6acb3ac4a7e5
4f8a30fa4a33bbef54acd1be270728a14913fe7b
describe
'info:fdaE20080623_AAAACEfileF20080623_AAAQSA-norm-0' 'aip-filesF20080623_AAAQSA-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
normalize
'54113' 'info:fdaE20080623_AAAACEfileF20080623_AAAQSB' 'sip-files00065.pro'
af276b57deef5b8d4a4c84d0d7ca5969
65dca9f64a7c62f970c0640b38205c4aa9a698fb
describe
'14301' 'info:fdaE20080623_AAAACEfileF20080623_AAAQSC' 'sip-files00065.QC.jpg'
eb868f61a941354ffe8a6a0646226de5
ba0a158fc9c007a8e75c91b6106f1b462020d027
describe
'937920' 'info:fdaE20080623_AAAACEfileF20080623_AAAQSD' 'sip-files00065.tif'
4a53a97a06636a134956249d1519e8d7
676e0f23f710ce6d1d30ec541fc18c92f562fd84
describe
'2894' 'info:fdaE20080623_AAAACEfileF20080623_AAAQSE' 'sip-files00065.txt'
36e6cbd15d757328a61ecd20e26897c7
f3e2d79e229abc2081141d715216d96ededcd7b7
describe
'4785' 'info:fdaE20080623_AAAACEfileF20080623_AAAQSF' 'sip-files00065thm.jpg'
4f8a811edf006f1f79ddeee302bdca6c
d327c732abd49533e7cda9e5faf7968ebb47c1b6
describe
'59809' 'info:fdaE20080623_AAAACEfileF20080623_AAAQSG' 'sip-files00066.jp2'
8bf3ce1787a59d107fe4aacedbc101d9
e092239b80887c9455346df4e4376de545ca49ce
describe
'28976' 'info:fdaE20080623_AAAACEfileF20080623_AAAQSH' 'sip-files00066.jpg'
cd86fa769d42d664f249a6f4fee641b2
964dd68d6495618e2ba82591c9115a1f122544ab
describe
'25529' 'info:fdaE20080623_AAAACEfileF20080623_AAAQSI' 'sip-files00066.pdf'
31ffd105717435bad0b35d07388b1d33
0e74fbd8d23934ae7498cb8692688f429ea944cf
describe
'info:fdaE20080623_AAAACEfileF20080623_AAAQSI-norm-0' 'aip-filesF20080623_AAAQSI-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
normalize
'37000' 'info:fdaE20080623_AAAACEfileF20080623_AAAQSJ' 'sip-files00066.pro'
63c2a4931f024aac60f13ca81a9aee32
9d9feb939815067c7795d4b2e522736ac75dd4a0
describe
'9786' 'info:fdaE20080623_AAAACEfileF20080623_AAAQSK' 'sip-files00066.QC.jpg'
d62e4445e647c15a45b029e7fd205238
c874e8757cb7a1df5ed26e1729972e44315152b0
describe
'950076' 'info:fdaE20080623_AAAACEfileF20080623_AAAQSL' 'sip-files00066.tif'
9c4ddd049b0cb8ce47b0f035f263f763
d66599735808d8201dfa294c891979d6166e46a9
describe
'2087' 'info:fdaE20080623_AAAACEfileF20080623_AAAQSM' 'sip-files00066.txt'
95bb58ed3086bf219a1c8a9cc207efb6
54578fb96de8510011af09e0230100ff0ac26e68
describe
'3129' 'info:fdaE20080623_AAAACEfileF20080623_AAAQSN' 'sip-files00066thm.jpg'
c1b855c16c75d4d06d3c24ca9cb58aa1
242c76442811736ab6ab2a9b17b995adc2fb83f3
describe
'71914' 'info:fdaE20080623_AAAACEfileF20080623_AAAQSO' 'sip-files00067.jp2'
cebe921147149c7b89aee24046f0305f
dca4523ae2eeebb42864e1d60650365739e793c4
describe
'32503' 'info:fdaE20080623_AAAACEfileF20080623_AAAQSP' 'sip-files00067.jpg'
fb61b9c8f35050cb6657a683ccaff895
1e0176e895d15549279245f3e12b96952c7a720a
describe
'30802' 'info:fdaE20080623_AAAACEfileF20080623_AAAQSQ' 'sip-files00067.pdf'
c4a6eddc272a45d67dc86f3184c47c5e
f9a79a413c8e64c37019c8699a56943359c03017
describe
'info:fdaE20080623_AAAACEfileF20080623_AAAQSQ-norm-0' 'aip-filesF20080623_AAAQSQ-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
normalize
'42460' 'info:fdaE20080623_AAAACEfileF20080623_AAAQSR' 'sip-files00067.pro'
6bd48d61245635a0a9b7abf7dd6d957c
80f23097e11f0494e44967e3b820304e23a18819
describe
'10950' 'info:fdaE20080623_AAAACEfileF20080623_AAAQSS' 'sip-files00067.QC.jpg'
f4b53b4b8c1bf78103a9efe9514c7edc
4cb0dc5c49ba74f7cefebd12313b048e40971716
'2017-03-09T11:25:21-05:00'
describe
'959648' 'info:fdaE20080623_AAAACEfileF20080623_AAAQST' 'sip-files00067.tif'
07911c65bccc395c1e7a5957df16e96e
ae393d5f987d984e1b0cfb6b76820323ab531ff8
describe
'2106' 'info:fdaE20080623_AAAACEfileF20080623_AAAQSU' 'sip-files00067.txt'
6ecb933a33bb00163300952821d43df9
9df2fd488319c6a66f46142570dbdb7202bdda06
describe
Invalid character
Invalid character
'3850' 'info:fdaE20080623_AAAACEfileF20080623_AAAQSV' 'sip-files00067thm.jpg'
d55940e6c47b8aed8edeef3b85658cdf
89c83f096390ba7c6a5c36951e3af1449b70e8e2
describe
'89146' 'info:fdaE20080623_AAAACEfileF20080623_AAAQSW' 'sip-files00068.jp2'
0468573c62b05e6b75d2af1f4fc79358
2ec283e9527add7fd1520674b8adfad47697607d
describe
'38474' 'info:fdaE20080623_AAAACEfileF20080623_AAAQSX' 'sip-files00068.jpg'
1fd578960a8c6582e208d929d1eba154
e544a87a9376c2af432936c411fba1a359562fc6
describe
'37837' 'info:fdaE20080623_AAAACEfileF20080623_AAAQSY' 'sip-files00068.pdf'
4b5696bdb0bd97b0c034bf8d233ab745
810b1c3b4583403c210bfcd109c628db72dca7f3
describe
'info:fdaE20080623_AAAACEfileF20080623_AAAQSY-norm-0' 'aip-filesF20080623_AAAQSY-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
normalize
'51415' 'info:fdaE20080623_AAAACEfileF20080623_AAAQSZ' 'sip-files00068.pro'
2c945f8c94fd620f5adde329ea6bffd4
854a780fb42701e8578eef32f3199e3fb2779e7d
describe
'13415' 'info:fdaE20080623_AAAACEfileF20080623_AAAQTA' 'sip-files00068.QC.jpg'
9f5fb62633b5ae5af2970ba97aa6863b
1b7d235d1ae0db13b1c87abc081977bd817cf14f
describe
'950236' 'info:fdaE20080623_AAAACEfileF20080623_AAAQTB' 'sip-files00068.tif'
208762c05d2d5f9ddc9c9066cb103070
3d4004c1620e136a509c95f824a0f5fdb7fdb728
describe
'3039' 'info:fdaE20080623_AAAACEfileF20080623_AAAQTC' 'sip-files00068.txt'
94ffb25b75d786ad64a3d4cc48c2b58c
565a94d3fe046415b9f8f5263cb1999faa93b736
describe
'4581' 'info:fdaE20080623_AAAACEfileF20080623_AAAQTD' 'sip-files00068thm.jpg'
16bdd712bd87caa38a4332948c358df8
001b6dab5bb6b8a71e03499ab1a856119ee34a8d
describe
'83660' 'info:fdaE20080623_AAAACEfileF20080623_AAAQTE' 'sip-files00069.jp2'
d5bed8d1ef9ad52d6ec65aa547a9aed3
a5b7784b946acbe27062c2c8dc38601bc8480173
describe
'38179' 'info:fdaE20080623_AAAACEfileF20080623_AAAQTF' 'sip-files00069.jpg'
a770880e76cb2143f9b7e4bb7655e17e
1235552d1b225cd51e38726499699b7a06a4672f
describe
'35049' 'info:fdaE20080623_AAAACEfileF20080623_AAAQTG' 'sip-files00069.pdf'
c4b6640121f75f95c9445a25c737238f
7d4aca97e5eed847f048035ad1a37eec45a5131b
describe
'info:fdaE20080623_AAAACEfileF20080623_AAAQTG-norm-0' 'aip-filesF20080623_AAAQTG-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
normalize
'47400' 'info:fdaE20080623_AAAACEfileF20080623_AAAQTH' 'sip-files00069.pro'
b8965df8f1a312f02ccae32258fa92ef
215763e1d20543b9ec01e0c69185149286c038af
describe
'14099' 'info:fdaE20080623_AAAACEfileF20080623_AAAQTI' 'sip-files00069.QC.jpg'
3e1ccf2869a155ad2f28887e2d9d68cc
b0ddef9a6a17c86968b23f457e67be20dcbca677
describe
'942356' 'info:fdaE20080623_AAAACEfileF20080623_AAAQTJ' 'sip-files00069.tif'
c0d4f898259cf18cba30bea94353be49
b78714f6bf155a5560be4774832b6a89d15e50d0
describe
'2469' 'info:fdaE20080623_AAAACEfileF20080623_AAAQTK' 'sip-files00069.txt'
387f8d6d0cfc362eb747a1d89851f836
1d5bf57f2181fc0dbc69a9fb80944df46a925e49
describe
'4585' 'info:fdaE20080623_AAAACEfileF20080623_AAAQTL' 'sip-files00069thm.jpg'
615b19db77747e3ff7fb895ada9ce364
49b88b3ad64b9812a615e02e45f9f1442d29a604
describe
'90555' 'info:fdaE20080623_AAAACEfileF20080623_AAAQTM' 'sip-files00070.jp2'
1dec06b5ae3128a9bae66bb60a28247e
86ee006b8d56362e72abd0ed03f808e7718647ce
describe
'39428' 'info:fdaE20080623_AAAACEfileF20080623_AAAQTN' 'sip-files00070.jpg'
4ffcaebbbf81e5962cde5a755991d634
bb0f7dc96dfe12cff3be3d84431847faa9fd9949
describe
'38999' 'info:fdaE20080623_AAAACEfileF20080623_AAAQTO' 'sip-files00070.pdf'
256e8389948305f1a8235c74e83e3f60
fc23510db55c17fe177a0644e0178c6f0cdd1458
describe
'info:fdaE20080623_AAAACEfileF20080623_AAAQTO-norm-0' 'aip-filesF20080623_AAAQTO-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
normalize
'52398' 'info:fdaE20080623_AAAACEfileF20080623_AAAQTP' 'sip-files00070.pro'
702f4c700e0afd41ad483952dbadd2e5
bb8d0c5baab1995f24b6466f3fabba6fe4f8799a
describe
'13695' 'info:fdaE20080623_AAAACEfileF20080623_AAAQTQ' 'sip-files00070.QC.jpg'
74cb6486c28ab48290104fc1e4850039
071a5506f2e460d1e674c7950de01ba0d8b64d03
describe
'932828' 'info:fdaE20080623_AAAACEfileF20080623_AAAQTR' 'sip-files00070.tif'
2c0a07cb2254cd03c451f6debdaf24da
65d5c9b5365d5a84202dbea0ef1cb8e3678a0fc1
describe
'3336' 'info:fdaE20080623_AAAACEfileF20080623_AAAQTS' 'sip-files00070.txt'
73a5a29eb2eaf9d62f65f73c90b7304a
d47ef37e1ad5f26e2bf6ec697efbd24008672cc0
describe
'4625' 'info:fdaE20080623_AAAACEfileF20080623_AAAQTT' 'sip-files00070thm.jpg'
9f6cf356526647dc80b8270bc283367d
2cac5979258192c121b82cc4aee370d30a7daf5b
describe
'83867' 'info:fdaE20080623_AAAACEfileF20080623_AAAQTU' 'sip-files00071.jp2'
c0ebfb44f08df03061c0ec9350b753ae
1fee139b003bf01cc584d90ea67a9512ab27fe71
describe
'39779' 'info:fdaE20080623_AAAACEfileF20080623_AAAQTV' 'sip-files00071.jpg'
551b5923b655316402c9d7c63c543c99
fbc250b244483a409bc3026b6154ba2342be027a
describe
'35833' 'info:fdaE20080623_AAAACEfileF20080623_AAAQTW' 'sip-files00071.pdf'
b7ab0a4919c409d6e10c088ca8d8e02f
613014f7d4fcc39ec62d9e975cae2c2790adab9c
'2017-03-09T11:28:08-05:00'
describe
'info:fdaE20080623_AAAACEfileF20080623_AAAQTW-norm-0' 'aip-filesF20080623_AAAQTW-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
normalize
'50004' 'info:fdaE20080623_AAAACEfileF20080623_AAAQTX' 'sip-files00071.pro'
576a7e95e03b824daf066c04d31b1a41
6f49a01946a92740cbbabc6e292e705055dcae48
describe
'14564' 'info:fdaE20080623_AAAACEfileF20080623_AAAQTY' 'sip-files00071.QC.jpg'
4044e59da9ab6248ae6dd3594207422f
0998aa6394d6911a9defeaeafc12c4b6cf668a73
describe
'965420' 'info:fdaE20080623_AAAACEfileF20080623_AAAQTZ' 'sip-files00071.tif'
61bd716818d5794a6ea3bd43c8c20a98
190019be56cfa7647df2ae94ce1bd32dffbcc836
describe
'2628' 'info:fdaE20080623_AAAACEfileF20080623_AAAQUA' 'sip-files00071.txt'
d3aa59e545ee479ee1f2a16eec7499a7
08ca783ef145d57118b0711732b8d8cefe596f0e
describe
'4633' 'info:fdaE20080623_AAAACEfileF20080623_AAAQUB' 'sip-files00071thm.jpg'
bf9e657398235975a5683ee3cbc2688e
3ca3cc27089bc5ca77097a0d863aee88c01ee23c
describe
'90415' 'info:fdaE20080623_AAAACEfileF20080623_AAAQUC' 'sip-files00072.jp2'
a97ef1c5696264f7d2dd0cfecef21319
41c81696f8bdec7145375ca4881843ea8f64c0de
describe
'39752' 'info:fdaE20080623_AAAACEfileF20080623_AAAQUD' 'sip-files00072.jpg'
ec770f8e649824da92e4bb4a1b8654f4
8540639c5669847f6e43922ba3396c4cc5cb3f5f
'2017-03-09T11:28:30-05:00'
describe
'38777' 'info:fdaE20080623_AAAACEfileF20080623_AAAQUE' 'sip-files00072.pdf'
b725a62fbfa2aa93f2fd75bf15e0fb20
f001d1adbcf63662dabdc6a29112ccf5c7ca164e
describe
'info:fdaE20080623_AAAACEfileF20080623_AAAQUE-norm-0' 'aip-filesF20080623_AAAQUE-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
normalize
'51217' 'info:fdaE20080623_AAAACEfileF20080623_AAAQUF' 'sip-files00072.pro'
4ad7badda5bdf7809e7b9e8272c01216
93de5e7853ae09947b606c2a086b795730b95304
describe
'14282' 'info:fdaE20080623_AAAACEfileF20080623_AAAQUG' 'sip-files00072.QC.jpg'
ddc23004485b369e154801dcf47e9482
49fc3600140c034ef2ef4f92d939d20d55a6048a
describe
'939048' 'info:fdaE20080623_AAAACEfileF20080623_AAAQUH' 'sip-files00072.tif'
5cf16aadbe97cbe1f94c93be5a04a9c5
0ae6613a7355b566045587deb8e32bce2d9e72b8
describe
'2906' 'info:fdaE20080623_AAAACEfileF20080623_AAAQUI' 'sip-files00072.txt'
18aee32bf0912f026a75570eef129d1b
237814243a5c0c3caf51eef1742a0021cba88d8d
describe
'4447' 'info:fdaE20080623_AAAACEfileF20080623_AAAQUJ' 'sip-files00072thm.jpg'
ac841963b7d1f411015fba2e6eade154
a4a0b1a16287f8ea1a69691a93c53ed3fe19ac4b
describe
'69009' 'info:fdaE20080623_AAAACEfileF20080623_AAAQUK' 'sip-files00073.jp2'
5f886ca14b6b5a13b0e2d67ed89308dd
82dfdb056927274580be0409c672461ca6aa6cfb
describe
'31515' 'info:fdaE20080623_AAAACEfileF20080623_AAAQUL' 'sip-files00073.jpg'
e145c9250be13ccdafa797ea0dd92491
ae3b162de6754e1d00530662b32bdc132b4b601f
describe
'29039' 'info:fdaE20080623_AAAACEfileF20080623_AAAQUM' 'sip-files00073.pdf'
3174369bc69a8a0dab61c2b0ce63d341
53c09811c9faedc74c31b948a471be8f658acb38
'2017-03-09T11:28:33-05:00'
describe
'info:fdaE20080623_AAAACEfileF20080623_AAAQUM-norm-0' 'aip-filesF20080623_AAAQUM-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
normalize
'37673' 'info:fdaE20080623_AAAACEfileF20080623_AAAQUN' 'sip-files00073.pro'
344217a18409ad5db5f9004dcf20f279
2537db2c426a5d8b8a662dd5a82e467e3d8bf28b
describe
'11542' 'info:fdaE20080623_AAAACEfileF20080623_AAAQUO' 'sip-files00073.QC.jpg'
4bf0b245d9d8555cc65be90d0023a263
822f4ac20a7dea1e6e76349a76dc1c2de5772e39
describe
'968996' 'info:fdaE20080623_AAAACEfileF20080623_AAAQUP' 'sip-files00073.tif'
a88aee2d25853464673a4287bb7bf1ec
98036b74862e09bc62204cfb01a946988abafb0f
describe
'1903' 'info:fdaE20080623_AAAACEfileF20080623_AAAQUQ' 'sip-files00073.txt'
bb0ad9fa5245419a2b8fe872e6004a2f
acd87df874a4ca4b083f002ba8985ef679461418
describe
'3768' 'info:fdaE20080623_AAAACEfileF20080623_AAAQUR' 'sip-files00073thm.jpg'
65e3750b8913f24d19ce9d1d14872f1e
138abdb74fc3ab8a11f6642c325c470d3722a810
describe
'86559' 'info:fdaE20080623_AAAACEfileF20080623_AAAQUS' 'sip-files00074.jp2'
401aeda7e4faeca73bf8651731a9de90
545cf5d72408867f557b5c9f29ab7d27d17a74e2
describe
'info:fdaE20080623_AAAACEfileF20080623_AAAQUT' 'sip-files00074.jpg'
1ece2f3dd8094b7c1b90802fc64cbd30
1ea8abf9af7aae3fb063dae1e5f3d6943fe4d8e3
describe
'36328' 'info:fdaE20080623_AAAACEfileF20080623_AAAQUU' 'sip-files00074.pdf'
f30d2624f691c43ef27cf26ab540cde9
0ee9c16d59244be69635478e451bad1a02baa53f
describe
'info:fdaE20080623_AAAACEfileF20080623_AAAQUU-norm-0' 'aip-filesF20080623_AAAQUU-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
normalize
'46948' 'info:fdaE20080623_AAAACEfileF20080623_AAAQUV' 'sip-files00074.pro'
123008c442829fe0d46f20e6f8d3578b
38549e5a112ea4b0f53fc12d221981e527020e2c
describe
'13638' 'info:fdaE20080623_AAAACEfileF20080623_AAAQUW' 'sip-files00074.QC.jpg'
6dc7d991e585ba5250b08afb7c33b39e
1dfddb4535aedcac8fa9434af63688e13e8f8651
describe
'957704' 'info:fdaE20080623_AAAACEfileF20080623_AAAQUX' 'sip-files00074.tif'
0611e7f0321cd8c9def7075b85f56f73
006de94432d889c46a51b9d68e930f116bf58028
describe
'2981' 'info:fdaE20080623_AAAACEfileF20080623_AAAQUY' 'sip-files00074.txt'
54ac6c5930160ceb289761590cebfab7
e7b3451b7b074507fb0fe2774c7462e04caf934f
describe
'4677' 'info:fdaE20080623_AAAACEfileF20080623_AAAQUZ' 'sip-files00074thm.jpg'
a6342421ed632db84b01f2a3e8696d35
7791349ee145a754f83e0dc728b254b50e57f60b
describe
'73236' 'info:fdaE20080623_AAAACEfileF20080623_AAAQVA' 'sip-files00075.jp2'
613146db92a0ab06e67b101d1db9cbe9
e054a59e3aa3a4c93efa3a64fcc469aa3e53456b
describe
'33898' 'info:fdaE20080623_AAAACEfileF20080623_AAAQVB' 'sip-files00075.jpg'
a1ecd1efbaa918eec5717b52281bbde4
de0be8748a219ab0f1aa3e745548ecec59b4dd91
describe
'30965' 'info:fdaE20080623_AAAACEfileF20080623_AAAQVC' 'sip-files00075.pdf'
b7fdca9886367eafe317d4456abec89e
7372261006c45aa4bc552f7840ad6d079cd46968
describe
'info:fdaE20080623_AAAACEfileF20080623_AAAQVC-norm-0' 'aip-filesF20080623_AAAQVC-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
normalize
'39341' 'info:fdaE20080623_AAAACEfileF20080623_AAAQVD' 'sip-files00075.pro'
21844d868b1663d5a7abd93cc0a89ded
25c0dea3d0f18a439607c2b5889c1e66f53d6261
describe
'12216' 'info:fdaE20080623_AAAACEfileF20080623_AAAQVE' 'sip-files00075.QC.jpg'
7d506aab9a3d5f2e3a0411c186d0a9fd
5d8e47739a96f5ea59d9d9170d5dee58511ce7c6
describe
'983436' 'info:fdaE20080623_AAAACEfileF20080623_AAAQVF' 'sip-files00075.tif'
2cdfcf550d488f2c37950e823253f8c7
0b947f469d2f93a9e4fbb5c81382ceb603233ae0
describe
'2002' 'info:fdaE20080623_AAAACEfileF20080623_AAAQVG' 'sip-files00075.txt'
c9e44cd80c335c3c237e5fe3393a177a
209e946e2ab7095d8391b4f0062f0ea40c1718fb
describe
'4291' 'info:fdaE20080623_AAAACEfileF20080623_AAAQVH' 'sip-files00075thm.jpg'
41b0014cab08e7fda48059b1e7a18fe6
dadbb78f1a0526f3fb5761c4f4eeb0e5df890ea9
describe
'82214' 'info:fdaE20080623_AAAACEfileF20080623_AAAQVI' 'sip-files00076.jp2'
5acc9f222dbd5d49fa2ee16a08767399
4070602ffe27ed29e38ee26c030b2eec294b8e4b
describe
'34902' 'info:fdaE20080623_AAAACEfileF20080623_AAAQVJ' 'sip-files00076.jpg'
09f4e8c1cecd71153a86da3c2bbb994c
f8d28884e57dfebea46957d1f3719d495bcc3876
describe
'35167' 'info:fdaE20080623_AAAACEfileF20080623_AAAQVK' 'sip-files00076.pdf'
261c6c265cba2f5b6d5ff63c8fd1f4d6
4ca49b164466a7f91a0bd68769c96f20d3a13f71
describe
'info:fdaE20080623_AAAACEfileF20080623_AAAQVK-norm-0' 'aip-filesF20080623_AAAQVK-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
normalize
'46042' 'info:fdaE20080623_AAAACEfileF20080623_AAAQVL' 'sip-files00076.pro'
64e96507b3b22402a72fa31e3253c1ba
546870115cdcb74d0014edde069b3741b1f90503
describe
'11763' 'info:fdaE20080623_AAAACEfileF20080623_AAAQVM' 'sip-files00076.QC.jpg'
9e3ac7f6b9e0231aca28f51b56749a8b
83477571753ff6c4d16b327c38ec9bc7fcc4c9c1
describe
'972856' 'info:fdaE20080623_AAAACEfileF20080623_AAAQVN' 'sip-files00076.tif'
91f9aefd7928099e8358c246124eccfb
0a4f5ab55fe0370e9c68d6d9ac9bb0432b1d8d6f
describe
'2975' 'info:fdaE20080623_AAAACEfileF20080623_AAAQVO' 'sip-files00076.txt'
2c000b022325e91c7fd72c33c9818baa
c6b0ceaf8cacbb4083de02b310ef628805edcb89
describe
'4012' 'info:fdaE20080623_AAAACEfileF20080623_AAAQVP' 'sip-files00076thm.jpg'
cc8354ea7a8cadefb286adb7729c101b
74626154e31b095eae1488f33e08c1f5eaaebb47
describe
'91612' 'info:fdaE20080623_AAAACEfileF20080623_AAAQVQ' 'sip-files00077.jp2'
29b127157b6938b509d52a7563660a26
352b7a87efd8ec8a594a9d094cd0bf7aeff9527c
describe
'40545' 'info:fdaE20080623_AAAACEfileF20080623_AAAQVR' 'sip-files00077.jpg'
fde1d54e60444d8cfe14fe42c8671c97
619a85115d7d0af58eb879144a181a0cdb75a042
describe
'38615' 'info:fdaE20080623_AAAACEfileF20080623_AAAQVS' 'sip-files00077.pdf'
70bb3eadb3f035763abd7f5cc3fd9a04
7cdf13f82c774e5dcb3106f18ec34ba3e4607f78
describe
'info:fdaE20080623_AAAACEfileF20080623_AAAQVS-norm-0' 'aip-filesF20080623_AAAQVS-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
normalize
'53716' 'info:fdaE20080623_AAAACEfileF20080623_AAAQVT' 'sip-files00077.pro'
d590c882cb93020e056079dea845fe09
abc8f63f4daf54c5d558db431f658f736f16e9b9
describe
'14491' 'info:fdaE20080623_AAAACEfileF20080623_AAAQVU' 'sip-files00077.QC.jpg'
9c0353392bb92ec32e5cd0d541a9de83
5b35b7bb0079e53d14b0288768f46194e6ea0295
describe
'978452' 'info:fdaE20080623_AAAACEfileF20080623_AAAQVV' 'sip-files00077.tif'
6dee9725d4a5d3806a63ebafe88286ec
5f6819ee1b63ac7625d7b376a3db2551193a2256
describe
'2916' 'info:fdaE20080623_AAAACEfileF20080623_AAAQVW' 'sip-files00077.txt'
29ccd80418f715ed4644b7ea9834b454
77f12914f7b17f3a6af0b507da37c4c88436d4e9
describe
'4721' 'info:fdaE20080623_AAAACEfileF20080623_AAAQVX' 'sip-files00077thm.jpg'
6f3f324eb593cdcead1cc3a86983a65a
c65dbe91002c77790f85d78b516597e6fd13d0c5
describe
'153168' 'info:fdaE20080623_AAAACEfileF20080623_AAAQVY' 'sip-filescopyright.jp2'
cd965abaafb5da42dc6c8def20d374f4
b811824c94aa0ae5a5f04cfb64b27e9e0927243a
describe
'103670' 'info:fdaE20080623_AAAACEfileF20080623_AAAQVZ' 'sip-filescopyright.jpg'
d028360928b6690b49cfe8211e6bb6a5
db68f5028a78f337081c164d3478ffd3e30a8a09
describe
'71602' 'info:fdaE20080623_AAAACEfileF20080623_AAAQWA' 'sip-filescopyright.pdf'
48729b50e74f3d43f6e6a9baba1417ac
21dd8a29344b70183d87ed795895da585eee2ca6
describe
'info:fdaE20080623_AAAACEfileF20080623_AAAQWA-norm-0' 'aip-filesF20080623_AAAQWA-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
normalize
'35816' 'info:fdaE20080623_AAAACEfileF20080623_AAAQWB' 'sip-filescopyright.pro'
09824414c5fc8565109bbbfc76cee5f5
126a0d690683cdc19c797452a11dfd7a91b7a4e1
describe
'35083' 'info:fdaE20080623_AAAACEfileF20080623_AAAQWC' 'sip-filescopyright.QC.jpg'
28180ee8185b27af4702a664eb2b5d1b
f0e1d4e0f0dcb1a265ec575f3d87a525ada2ad6d
describe
'1060432' 'info:fdaE20080623_AAAACEfileF20080623_AAAQWD' 'sip-filescopyright.tif'
a74ea382978e92381226fd9282282c91
53932ccb28c0275c4bb45111fc084707a573eae9
describe
'1329' 'info:fdaE20080623_AAAACEfileF20080623_AAAQWE' 'sip-filescopyright.txt'
15f2bbd34b776d39b92ffb1c4f760b27
b0251f2ed30996bc7ed3d8efa687abc9a6800fa9
describe
Invalid character
Invalid character
'10085' 'info:fdaE20080623_AAAACEfileF20080623_AAAQWF' 'sip-filescopyrightthm.jpg'
b0566b6a6e9b9bfb3fa924203ff11cf8
63d705588c1580afc86f43138330df2fe31f906d
describe
'4712506' 'info:fdaE20080623_AAAACEfileF20080623_AAAQWG' 'sip-filesUF00001159.pdf'
3204978e635e59fcd874de5baed48cf8
039e29c79b8699e9b12d8fcf4e6d68425073a02f
'2017-03-09T11:27:28-05:00'
describe
'info:fdaE20080623_AAAACEfileF20080623_AAAQWG-norm-0' 'aip-filesF20080623_AAAQWG-norm-0.pdf'
8cbf40949b8b639101cd4e2c803d9b62
6e3842fc6d7fb92b4cf6a2346c8099c7289050d2
describe
'2017-03-09T11:27:37-05:00'
normalize
'131565' 'info:fdaE20080623_AAAACEfileF20080623_AAAQWH' 'sip-filesUF00001159_00001.mets'
a30d49518773723c09492ab8a6f37d36
3a9f7f6403beb60550c61ab339cf8f40f657775c
describe
TargetNamespace.1: Expecting namespace 'http://www.uflib.ufl.edu/digital/metadata/ufdc2/', but the target namespace of the schema document is 'http://digital.uflib.ufl.edu/metadata/ufdc2/'.
'2017-03-09T11:29:56-05:00' 'mixed'
xml resolution
http://www.loc.gov/standards/xlink.xsd
BROKEN_LINK schema http://www.loc.gov/standards/xlink.xsd
TargetNamespace.1: Expecting namespace 'http://www.uflib.ufl.edu/digital/metadata/ufdc2/', but the target namespace of the schema document is 'http://digital.uflib.ufl.edu/metadata/ufdc2/'.
'187294' 'info:fdaE20080623_AAAACEfileF20080623_AAAQWK' 'sip-filesUF00001159_00001.xml'
4c32fd3be5df8d236ab73afbae39cdee
a14ef82c2183b1cdc4614b2b3bf76a1c7569ffe8
describe
'2017-03-09T11:29:57-05:00'
xml resolution
http://www.loc.gov/standards/xlink.xsd
http://www.loc.gov/standards/xlink.xsd


xml version 1.0 encoding UTF-8
REPORT xmlns http:www.fcla.edudlsmddaitss xmlns:xsi http:www.w3.org2001XMLSchema-instance xsi:schemaLocation http:www.fcla.edudlsmddaitssdaitssReport.xsd
INGEST IEID ERS5UI9N6_6Z2UA5 INGEST_TIME 2017-04-19T18:41:05Z PACKAGE UF00001159_00001
AGREEMENT_INFO ACCOUNT UF PROJECT UFDC
FILES