Northern Plains Craterforms: Evidence for the Accumulation and Degradation of Paleo-Mantles

Physics

Scientific paper

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Scientific paper

An inventory of lowland craterforms may be remnants of a ~35-m-thick,
Amazonian-age paleo-mantle at mid- to high-latitude. Our observations
suggest most lowland craterforms are not volcanic in origin but rather
impact craters that were modified due to cyclic mantling and exhumation.

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