Ferrous Minerals and Impactite Mineralization at Missouri's Crooked Creek and Decaturville Impact Craters

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Scientific paper

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Scientific paper

Epigenetic hydrothermal mineralization, subsequent to the Crooked Creek
and Decaturville impacts, accompanied Paleozoic dolomitization of
carbonates at a regional scale in the Ozarks and produced quantities of
ferrous minerals at both locations.

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