Lake Bosumtwi Drilling Project: Shock Metamorphism in Rocks from Core BCDP-8A vs. Experimental Data

Physics

Scientific paper

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Scientific paper

Recovery experiments with carbonaceous greywackes at 34, and 39.5 GPa
confirm that the generally low shock levels recorded in lithologies
inside the Lake Bosumtwi crater, are not due to specific petrophysical
properties of this lithology yet may be caused by the obliquity of the
impact.

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