Fig. 5From: Omori-like slow decay (p < 1) of postseismic displacement rates following the 2011 Tohoku megathrust earthquakeDistribution of the reference of convergence time of postseismic deformation in the horizontal components, \(t_{c}\), as time of \(d\left( t \right) =\) 1 cm/year (a typical value of tectonic deformation)Back to article page