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Evolution of a Late Cenozoic Supradetachment Basin Above a Flat-On-Flat Detachment With a Folded Lateral Ramp, SE Idaho
Uplift and exposure of the Bannock detachment system and the synextensional basin fill deposits of the Salt Lake Formation provide a unique exposure of the three-dimensional geometries of a low-angle normal fault system and the stratal architecture of the overlying supradetachment basin. Within this
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