Fig. 7.From: Source process of the 2011 off the Pacific coast of Tohoku Earthquake inferred from waveform inversion with long-period strong-motion recordsComparison of the contribution of the slip at each area shown in Fig. 4 to the waveforms at TMR, KSN and IBRH19. Traces 1, 2, and 3 are the synthetics calculated from Area 1, 2, and 3 of the fault model (Fig. 4).Back to article page