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

<div>Three components of the surface deformation for the homogenous-heterogeneous and zero topography-topography model. Left to right are displacement Ux, Uy, and Uz. (a–c) Homogenous-zero topography model (HOM-topo0). (d–f) Homogeneous model-topography model. (g–i) Heterogeneous-zero topography model. (j–l) Heterogeneous-topography model. Scale bar shows the displacement value in meter.</div>

International Journal of Geophysics

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Figure 5

Figure 5: Coseismic Deformation Responses due to Geometrical Structure and Heterogeneity of the Accretionary Wedge: Study Case 2010 Mentawai Earthquake, West Sumatra, Indonesia 

Figure 5 | Coseismic Deformation Responses due to Geometrical Structure and Heterogeneity of the Accretionary Wedge: Study Case 2010 Mentawai Earthquake, West Sumatra, Indonesia 