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Progress in Earth and Planetary Science
Fig. 14 | Progress in Earth and Planetary Science

Fig. 14

From: Seismicity distribution in the Tonankai and Nankai seismogenic zones and its spatiotemporal relationship with interplate coupling and slow earthquakes

Fig. 14

Observed waveforms in the vicinity of each station. a Examples of the observed waveform (horizontal component) whose focal depth is larger than the epicentral distance with respect to the hypocenter depth. The maximum epicentral distance for each station is shown in each figure. All waveforms are aligned by the P-wave arrival time. Blue lines show the approximate straight line of the S-wave arrival time. The thick green line shows the depth of the plate interface beneath each station. b Station locations shown in a. The focal mechanism solution for the 2016 off-Mie earthquake is also shown

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