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Fig. 13 | Progress in Earth and Planetary Science

Fig. 13

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. 13

Schematic representation of the vertical-temporal change of seismicity in the outer-rise region. Blue and red stars denote the normal-faulting and reverse-faulting small seismicity shown by previous studies (Seno and Gonzalez 1987; Hino et al. 2009; Obana et al. 2012, 2014, 2015). Note that the aftershocks occurred around the Mw 7.6 outer-rise ~40 min after the Tohoku-Oki earthquake (Obana et al. 2012) are located ~60 km east from the focal area of the 2012 doublet earthquake

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