Department or Administrative Unit
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.
McClusky, S. C.; Bjornstad, S. C.; Hager, B. H.; King, R. W.; Meade, B. J.; Miller, M. Meghan; Monastero, F. C.; and Souter, B. J., "Present Day Kinematics of the Eastern California Shear Zone from a Geodetically Constrained Block Model" (2001). All Faculty Scholarship for the College of the Sciences. 283.
Geophysical Research Letters
Copyright 2001 by the American Geophysical Union.