Fig. 5From: A new mechanical perspective on a shallow megathrust near-trench slip from the high-resolution fault model of the 2011 Tohoku-Oki earthquakeTemporal evolution of the slip. a Configuration of the temporal elements of the inversion analysis. b Slip amount of the subfaults in each temporal element. b Temporal evolution of the total slip amount, calculated by the summation of the temporal elementsBack to article page