| http://www.w3.org/ns/prov#value | - A 2-D profile across the Shanchiao Fault is chosen for elastic half-space dislocation modeling, and the results suggest that the fault is listric in the shallow crust with an abrupt change from subvertical ramp (85???-75???) to near-horizontal flat (10???-15???) at 3-4 km depth, consistent with an origin from the inversion of an orogen-related thrust detachment.
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