Coseismic Deformation Responses due to Geometrical Structure and Heterogeneity of the Accretionary Wedge: Study Case 2010 Mentawai Earthquake, West Sumatra, Indonesia

Figure 7

The vertical deformation at the cross-section shown in Figure 1. The flat vs topography model with homogeneous and heterogeneous medium. (b) The wedge dimension variation model. (c) The model with constant Vp/Vs 1.6 and Vp variation 5.1-5.7 km/s. (d) The model with constant Vp/Vs 2.2 and Vp variation 5.1-5.7 km/s. (e) The model with constant Vp 5.1 km/s and Vp/Vs variation 1.6-2.2. (f) The model with constant Vp 5.7 km/s and Vp/Vs variation 1.6-2.2.