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Cenozoic unconformities and depositional supersequences of North Atlantic continental margins: Testing the Vail model

C. Wylie Poag·Lauck W. Ward
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Abstract

Integrated outcrop, borehole, and seismic reflection stratigraphy from the U.S. and Irish margins of the North Atlantic basin reveals a framework of Cenozoic depositional supersequences and interregional unconformities that resembles the Vail depositional model. Paleo-bathymetric and paleoceanographic analyses of associated microfossil assemblages indicate a genetic link between the depositional framework and the relative position of sea level.

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C. Wylie Poag, Lauck W. Ward. 1987. Cenozoic unconformities and depositional supersequences of North Atlantic continental margins: Testing the Vail model. https://doi.org/10.1130/0091-7613(1987)15%3C159%3Acuadso%3E2.0.co%3B2

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