Modeling surface deformations at complex strike‐slip plate boundaries

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Abstract
Two new versions of the physical base‐traction model of Li and Rice (1987) have been developed to study the loading processes and surface deformation near plate boundaries with geometric complexities, including a shallow creeping fault segment and two subparallel faults. Predictions of surface velocity and surface slip rate for the region between the San Andreas fault and the Pacific coast at the latitude of the Parkfield‐Cholame segment using model parameters based on geologic, geodetic, and seismic considerations were found to be in good agreement with contemporary geodetic field data (not used in constraining model parameters). Also, predicted surface velocity for the Salton Sea‐Coachella Valley area were fit to recently derived contemporary geodetic data and very large baseline interferometry data, although here the model parameters are not well constrained.