Figure 4From: Contributions of poroelastic rebound and a weak volcanic arc to the postseismic deformation of the 2011 Tohoku earthquakePE in the upper crust. (a) PE only in upper 6 km of continental crust. (b) PE only in upper 16 km of the oceanic plate. (c) PE in both continental and oceanic crusts, i.e., the combined effect of (a) and (b). Colored contours and black arrows are vertical and horizontal displacements, respectively.Back to article page