Fig. 15From: Heterogeneous rheology of Japan subduction zone revealed by postseismic deformation of the 2011 Tohoku-oki earthquakea Total strain by viscous flow during ~ 5 years of postseismic deformation along the Miyagi-Yamagata region and the Fukushima-Niigata region (after Dhar et al. 2022). b The two-dimensional projection of modeled displacements from September 2012 to May 2016 along the Miyagi-Yamagata region and Fukushima-Niigata regionBack to article page