Fig. 2From: Strong localized asperity of the 2011 Tohoku-Oki earthquake, JapanWaveform fits obtained from the waveform inversion of the Tohoku-Oki earthquake. Black solid and red dotted lines represent the observed and synthetic waveforms, respectively. Waveforms with low signal-to-noise ratios, which were not used in the inversion, are not shown.Back to article page