Fig. 10From: Fault model of the 2012 doublet earthquake, near the up-dip end of the 2011 Tohoku-Oki earthquake, based on a near-field tsunami: implications for intraplate stress stateComparison of the observed (gray) and calculated (red) waveforms based on the superposition of the optimum fault models of subevents 1 and 2Back to article page