Fig. 5From: Heterogeneous rheology of Japan subduction zone revealed by postseismic deformation of the 2011 Tohoku-oki earthquakeThe postseismic evolution of effective viscosity in the power-law base model. The effective viscosities of steady-state (Maxwell element; left panel) and transient (Kelvin element; right panel) deformation are shown for a–b 1 day, c–d 1 year, e–f 3 years after the earthquakeBack to article page