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View article: Polyphase kinematic history of transpression along the Mecca Hills segment of the San Andreas fault, southern California
Polyphase kinematic history of transpression along the Mecca Hills segment of the San Andreas fault, southern California Open
Miocene–Pliocene sedimentary rocks in the Mecca Hills, southern California, were uplifted and deformed by transpression along a restraining bend in the San Andreas fault trace between the Orocopia and San Bernardino Mountains in Pleistocen…