Fig. 7From: Omori-like slow decay (p < 1) of postseismic displacement rates following the 2011 Tohoku megathrust earthquakeComparison between the evolution of the horizontal ground displacement rates (Fig. 2) and a Maxwellian viscoelastic simulation (Suito 2017) after the 2011 Tohoku Earthquake. The green points represent the simulation results of Model 4 (final model) in Suito (2017)Back to article page