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Folded and Faulted Salt Lake Formation Above the Miocene to Pliocene New Canyon and Clifton Detachment Faults, Malad and Bannock Ranges, Idaho: Field Trip Guide to the Deep Creek Half Graben and Environs
Previous studies identified a major detachment terrane in southeast Idaho in the Oxford Ridge area of the Bannock Range. This study shows that these top-to-the-WSW detachment faults are late Cenozoic in age, not Mesozoic to early Tertiary as previously inferred. Provenance and facies patterns in the
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