Fig. 5.From: Source process of the 2011 off the Pacific coast of Tohoku Earthquake inferred from waveform inversion with long-period strong-motion recordsComparison of observed (black) and synthetic (red) velocity waveforms. The origin of the time axis is the arrival of the P-wave. The pass-band of the band-pass filter is from 200 s to 20 s. Note that the order of the records is from north to south.Back to article page