Stratigraphy and Tertiary development of the continental margin east of Florida
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Stratigraphy and Tertiary development of the continental margin east of Florida

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Published by U.S. Govt. Print. Off. in Washington .
Written in English

Subjects:

  • Geology, Stratigraphic -- Tertiary.,
  • Geology -- Atlantic coast (United States),
  • Continental margins -- Florida.

Book details:

Edition Notes

Bibliography: p. 25.

Statementby John Schlee.
SeriesDrilling on the continental margin off Florida, Professional paper (United States. Geological Survey) -- 581-F
ContributionsGeological Survey (U.S.)
Classifications
LC ClassificationsQE691 .S34
The Physical Object
Pagination25 p. :
Number of Pages25
ID Numbers
Open LibraryOL14718676M

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  The period when prograding seems to be most active, was a time when extensive bed s of phosphorite were also deposited along the continental margin of the east coast of the U.S., in particular in northern Florida (Riggs, ) indicating a local increase in the nutrient content of the waters. This was the time when the largest shark ever (over. In the east faults of a continental hinge line offset continental blocks up to a kilometer. This structural boundary of the continent had been active until the Tertiary and formed listric growth faults in the Cretaceous section north of by: "Sequence Stratigraphy of a Continental Margin Subjected to Low-Energy and Low-Sediment-Supply Environmental Boundary Conditions: Late Pleistocene–Holocene Deposition Offshore Alabama, U.S.A.", Late Quaternary Stratigraphic Evolution of the Northern Gulf of Mexico Margin, John B. Anderson, Richard H. Fillon. Download citation file: Ris (Zotero). Mesozoic development and structure of the continental margin off South Carolina (USA). East Florida Lophelia Reefs-echosounder transects along .

East of the Pelagian Shelf the geology of the continental margin changes dramatically. The shallow shelf is replaced in the Gulf of Sirt by a typical continental margin of slope and rise. In effect, the offshore Gulf of Sirt is divided into two provinces by the Sabratah-Cyrenaica Fault Zone (Figure ). The area south of the fault is a. Quaternary coastal lithofacies, sequence development and stratigraphy in a passive margin setting, North Carolina and Virginia, USA February Sedimentology 60(2) The Tertiary coastal plain of panhandle Florida is approximately kilometers wide (Fig. 5), compared to approximately kilometers for east Texas. The average gradient along the entire reach of the Apalachicola River is m/km (Donoghue, ). Abstract. Shallow subsurface Tertiary sediments of mid-latitude, modern continental margins of the world contain a tremendously extensive and poorly known Neogene sediment sequence that has a high theoretical potential for containing major Cited by: 7.

@article{osti_, title = {Carbonate platform development in northeast Australia}, author = {Davies, P.J. and Symonds, P.A. and Feary, D.A. and Pigram, C.J.}, abstractNote = {In northeast Australia, the Great Barrier Reef and the Queensland and Marion plateaus comprise carbonate platforms separated by major rift basins. Cenozoic platform evolution has been dependent .   A Brief Tectonic History of the Arabian basin. The vast hydrocarbon accumulation s of the basin. Basin s of the Upper Jurassic are directly tied to the tectonic evolution of the Arabian Plate. This section attempts to trace the development of the northeast margin of the Arabian Plate a development accumulation the vast accumulation of the source, reservoir, and . His research extends from inland river, lake, and pocosin environments, to estuarine and barrier island systems, and seaward across the continental shelf. His areas of interest lie in sedimentation, Quaternary and Tertiary stratigraphy, coastal and mineral resources, and their inter-relationship with the development of human civilization. Dr. Stratigraphy and structure of Paleozoic outer continental-margin rocks in Pilot Knob Valley, north-central Mojave Desert, California / (Washington: U.S. G.P.O. ; Denver, CO: For sale by Book and Open-File Report Sales, U.S. Geological Survey, ), by Michael D. .