Fig. 12From: 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 with the result of Inazu and Saito (2014). a Tsunami source model of Inazu and Saito (2014). b Cross-section of the tsunami sources from this study (red line) and Inazu and Saito (2014) (blue) at 37.8°N. c Comparison of the observed waveforms (gray) and synthesized waveforms. Blue dashed and red lines are synthesized using the tsunami source model of the present study and Inazu and Saito (2014), respectivelyBack to article page