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Earth, Planets and Space
Fig. 6. | Earth, Planets and Space

Fig. 6.

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

Fig. 6.

Calculated final slip distribution and moment release rate for Model-1 in comparison with the moment-rate function in the slip inversion result (Yoshida et al., 2011). We assume that the dip angle of the plate interface is 20°, and the epicenter of the 2011 Tohoku earthquake is located at 38.1°N, 143.86°E (the value determined by JMA).

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