Fig. 3From: 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 stateResults of tsunami source inversion. a Distribution of the tsunami source. Contour line interval is 5 cm. b Comparison of the observed (gray) and synthesized (red) waveforms. Thick black lines denote the time window used for the inversionBack to article page