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STRUCTURAL ANALYSIS OF THE TENSLEEP FAULT, BIGHORN BASIN, WYOMING (PALEOSTRESS, FORELAND, JOINTS)
Bighorn basin the Precambrian fault smooth surface rock rock
2014/10/22
The Tensleep Fault is an east-west trending Precambrian fault reactivated during the Laramide orogeny. This study of the fault west of the base of the Bighorn Mountains involves three levels of analys...