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Progress in Earth and Planetary Science
Fig. 9 | Progress in Earth and Planetary Science

Fig. 9

From: Fault model of the 2012 doublet earthquake, near the up-dip end of the 2011 Tohoku-Oki earthquake, based on a near-field tsunami: implications for intraplate stress state

Fig. 9

Summary of the fault modeling. a Sea-surface height distribution calculated from the superposition of the those from the fault models of subevents 1 and 2. Locations of the optimum faults are also shown. b The moment rate function used for the teleseismic waveform calculation. c Aftershock distribution on the fault plane of subevent 2. Aftershocks with distances from the fault plane smaller than 5 km are shown. d, e Vertical profile along A-A’ and B-B’ lines in a. Orange and blue rectangles are the optimum fault models of subevents 1 and 2, respectively. Aftershocks are taken from the rectangular areas in a

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