Fig. 3.From: Centroid-moment-tensor analysis of the 2011 off the Pacific coast of Tohoku Earthquake and its larger foreshocks and aftershocksWaveform fits for the M W = 9.1 mainshock. Displacement waveforms are filtered between 500 and 1000 s, outside the range used in the inversion. Black lines are observed seismograms and red lines are corresponding normal-mode synthetic waveforms. Timescale shows time after the mainshock hypocentral time. For each pair of traces, the station name, channel, epicentral distance, and maximum displacement are given.Back to article page