Fig. 5.From: A scenario for the generation process of the 2011 Tohoku earthquake based on dynamic rupture simulation: Role of stress concentration and thermal fluid pressurizationThe evolution of coseismic slip for Model-1. Note that the color scale in each figure is not the same. (i) Snapshot at 10 s after the rupture start. (ii) At 20 s. (iii) At 30 s. (iv) At 40 s. (v) At 50 s. (vi) Final slip distribution.Back to article page