Fig. 4.From: Source process of the 2011 off the Pacific coast of Tohoku Earthquake inferred from waveform inversion with long-period strong-motion recordsUpper: Distributions of coseismic slip obtained for the 2011 Tohoku Earthquake. The star indicates the rupture starting point. The rectangle represented by the dashed line indicates 3 areas, Area 1, 2, and 3 denoted in the text. Lower: Distributions of peak moment rate together with the slip rate function at each subfault.Back to article page