Abstract:The San Andreas Fault (SAF) is one of the dominant components of the transform boundary between the Pacific and the North American Plate. Although the fault is verticalto sub-vertical at shallow (<10 km) depth, it variably dips at angles of ca. 40-70º to the southwest near the western Transverse Range and to the northeast in its southern segment at depths of ca. 10-20 km, and thus can be described as having a listric geometry at the crustal scale. The mechanism controlling the fault dip direction variation at … Show more
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