File:Map and regional seismic sections showing location of Nadir Crater.jpg

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English: "(A) Regional bathymetry map of the Guinea Plateau and Guinea Terrace showing location of 2D seismic reflection and well data used in this study. JS, Jane Seamount; NS, Nadir Seamount; PS, Porter Seamount. The white dashed line shows the NE extent of high-amplitude discontinuous seismic facies at the top Maastrichtian interpreted as ejecta deposits and associated tsunami deposits. The north-east limit of this facies closely corresponds with the Maastrichtian shelf-slope break at the landward margin of the Guinea Terrace. Inset map shows a paleogeographic reconstruction of the Atlantic near the end of the Cretaceous, ~66 Ma ago, made using GPlates software (58). Ch, Chicxulub Crater; Nd, Nadir Crater; Bo, Boltysh Crater. (B). Regional composite 2D seismic reflection profile extending from the GU-2B-1 well in the east to the deep Atlantic basin in the west, showing the structural and stratigraphic character of the Guinea Plateau and Guinea Terrace. (C) North-South seismic profile from the salt basin in the north to the Nadir Seamount, south of the Guinea Fracture Zone. Data courtesy of the Republic of Guinea and TGS."
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来源 https://www.science.org/doi/10.1126/sciadv.abn3096
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Authors of the study: Uisdean Nicholson https://orcid.org/0000-0003-0746-8549 Veronica J. Bray https://orcid.org/0000-0002-7277-3980 Sean P. S. Gulick https://orcid.org/0000-0003-4740-9068 and

Benedict Aduomahor https://orcid.org/0000-0002-6927-5892

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From the study "The Nadir Crater offshore West Africa: A candidate Cretaceous-Paleogene impact structure"

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