Fig. 13From: Heterogeneous rheology of Japan subduction zone revealed by postseismic deformation of the 2011 Tohoku-oki earthquakeThe effective viscosity of steady-state (left) and transient creep (right) estimated by Agata et al. (2019). a 0Â year, b 2.8Â years after the earthquake. The profile is along the Miyagi-Yamagata areasBack to article page