Geology of continental shelf, Onslow Bay, North Carolina, as revealed by submarine outcrops

Blake W. Blackwelder; Ian G. Macintyre; Orrin H. Pilkey

doi:10.1306/03b59a1c-16d1-11d7-8645000102c1865d

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Geology of continental shelf, Onslow Bay, North Carolina, as revealed by submarine outcrops

Blake W. Blackwelder·Ian G. Macintyre·Orrin H. Pilkey

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Abstract

Lithologic and stratigraphic data from rocks dredged from the continental shelf off Onslow Bay, North Carolina, provide surface control for seismic studies of the southeastern United States continental margin and help to explain the distribution of potentially economic phosphate-rich sediments on this shelf. Outcropping Miocene rocks in this area indicate that the region has long been a positive geologic feature and has received relatively little Pliocene and Pleistocene sedimentation. -from Authors

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American Association of Petroleum Geologists Bulletin Article

Source-reported bounding extent: 33.75214968374051° to 34.79157094249153° latitude; -78.03355465391473° to -76.44373147728382° longitude. This indicates report coverage, not an exact sampling location. View area on OpenStreetMap.

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Blake W. Blackwelder, Ian G. Macintyre, Orrin H. Pilkey. 1982. Geology of continental shelf, Onslow Bay, North Carolina, as revealed by submarine outcrops. https://doi.org/10.1306/03b59a1c-16d1-11d7-8645000102c1865d

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