Fig. 7.From: A scenario for the generation process of the 2011 Tohoku earthquake based on dynamic rupture simulation: Role of stress concentration and thermal fluid pressurization(i) Locations of point 1 (P1) and point 2 (P2) on the fault. (ii) Evolution of the slip velocity υ and the effective normal stress σ –p at P1 and P2. (iii) Evolution of the frictional strength τfs, the loading stress τfs, and the shear stress τsh at P2.Back to article page