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Progress in Earth and Planetary Science
Fig. 7 | Progress in Earth and Planetary Science

Fig. 7

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. 7

Sea-surface height changes from the models in the present study. a The tsunami source model with contour intervals of 5 cm. The rectangular area enclosed by the blue dashed lines denotes the area used for the fault modeling of subevent 2. b Subevent 2 fault model; the optimum fault is also shown. c the residual between a and b. CMT solutions for subevent 1 by GCMT, Lay et al. (2013) and Harada et al. (2013) are also shown. The rectangular area enclosed by the blue dashed lines is the area used for the fault modeling of subevent 1. d the subevent 1 fault model; the optimum fault is also shown

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