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Earth, Planets and Space
Fig. 2. | Earth, Planets and Space

Fig. 2.

From: Source process of the 2011 off the Pacific coast of Tohoku Earthquake with the combination of teleseismic and strong motion data

Fig. 2.

(a) P wave waveform fits for the teleseismic inversion. Selected stations used in the inversion are displayed, with observed and calculated waveforms shown as black (top) and red (lower) lines, respectively. The number above the station code is the peak-to-peak amplitude of the observed waveform (micro-meter) and the number below the station code is the source-to-station azimuth and epicentral distance. (b) Distribution of stations, with red circles representing epicentral distances between 30° and 100° from the mainshock in 10° increments.

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