Fig. 11From: Numerical earthquake model of the 20 April 2015 southern Ryukyu subduction zone M6.4 event and its impact on seismic hazard assessmentThe normalized ShakeMaps (norm of the three components PGA) of four test cases: a a full 3D velocity model with an inverted finite-fault source model, b a homogeneous half-space model (flat surface) with an inverted finite-fault source model, c a homogeneous half-space model (flat surface) with a double-couple point source, and d a homogeneous half-space model (flat surface) with an explosive sourceBack to article page