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Evidence For Late Miocene-Quaternary Low-Angle Oblique Strike-Slip Faulting on the West Salton Detachment Fault, Southern California
Low rakes of slickenlines, fault-strike-parallel anticlines, and basin fill that thins toward the West Salton detachment fault (WSDF) all show that the WSDF is not an ordinary low-angle normal fault near Yaqui Ridge in the western Salton Trough. Detailed geologic mapping along the western margin of
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