Chesapeake Bay Impact Crater: Seismostratigraphy and Lithostratigraphy of Displaced Sedimentary Megablocks

Physics

Scientific paper

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Scientific paper

Two new deep coreholes into basement in the Chesapeake Bay impact crater
confirm that displaced megablocks in the annular trough are dominated by
Cretaceous sediments and are detached from the crystalline basement
surface by a zone of shock-generated collapse.

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