Abstract:The movement and deformation of the Earth's crust and upper mantle provide critical insights into the evolution of earthquake processes and future earthquake hazards. Crustal deformation can be modeled by dislocation models that represent an earthquake fault in the crust as a defect in a continuum medium. Forward and inverse modeling have been performed using various analytical methods based on Green's function for linear responses and numerical methods that discretize model regions or boundaries. In this stud… Show more
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