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- W2121858500 abstract "According to the slip partitioning concept, the trench parallel component of relative plate motion in regions of oblique convergence is accommodated by strike-slip faulting in the overriding continental lithosphere. The pattern of postseismic surface deformation due to viscoelastic flow in the lower crust and asthenosphere following a major earthquake on such a fault is modified from that predicted from the conventual elastic layer over viscoelastic halfspace model by the presence of the subducting slab. The predicted effects, such as a partial suppression of the postseismic velocities by 1 cm/yr or more immediately following a moderate to great earthquake, are potentially detectable using contemporary geodetic techniques." @default.
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- W2121858500 date "2000-10-01" @default.
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- W2121858500 title "Viscoelastic Postseismic Rebound from Strike-Slip Earthquakes in Regions of Oblique Plate Convergence" @default.
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- W2121858500 doi "https://doi.org/10.1785/0119990136" @default.
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