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Progress in Earth and Planetary Science
Fig. 11 | Progress in Earth and Planetary Science

Fig. 11

From: 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 state

Fig. 11

Results of the forward calculation of the teleseismic waveforms based on the optimum fault model. a Locations of the teleseismic stations. b Comparison of the teleseismic waveforms. Black lines are the observed waveforms, and the synthetic waveforms using the velocity structure with and without the water layer are shown by red and blue lines, respectively. The bandpass filter of 10–500 s is applied

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