We compute the static displacement. stress. strain and the Coulomb failure stress produced in an elastic medium by a finite size rectangular fault after its dislocation with uniform stress drop but a non uniform dislocation on the source. The time-dependent rate of triggered earthquakes is estimated by a rate-state model applied to a uniformly distributed population of faults whose eq... https://www.missouriquiltcoes.shop/product-category/missouri-star-publications/
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