Present day kinematics of the Eastern California shear zone from a geodetically constrained block model

Abstract

We use Global Positioning System (GPS) data from 1993-2000 to determine horizontal velocities of 65 stations in eastern California and western Nevada between 35° and 37° N. We relate the geodetic velocities to fault slip rates using a block model that enforces path integral constraints over geologic and geodetic time scales and that includes the effects of elastic strain accumulation on faults locked to a depth of 15 km. The velocity of the Sierra Nevada block with respect to Nevada is 11.1 ± 0.3 mm/yr, with slip partitioned across the Death Valley, (2.8 ± 0.5 mm/yr), Panamint Valley (2.5 ± 0.8 mm/yr), and Airport Lake/Owens Valley (5.3 ± 0.7/4.6 ± 0.5 mm/yr) faults. The western Mojave block rotates at 2.1 ± 0.8°/My clockwise, with 3.7 ± 0.7 mm/yr of left lateral motion across the western Garlock Fault. We infer 11 ± 2 mm/yr of right lateral motion across the Mojave region of the Eastern California Shear Zone.