Earthquake simulation of the 2011 Mw9.0 Tohoku earthquake.

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The 2011 Mw9.0 Tohoku (Japan) earthquake is characterized by multi-scale heterogeneity of plate interface. The dynamic rupture simulation explains how this mega-earthquake starts, develops and propagates to M9.0 event. After Aochi and Ide (EPS, 2011), Ide and Aochi (Tectonophys. 2013).
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