Fig. 4From: 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 stateSea-surface displacement expected from the GCMT solution. Displacements from a the tsunami source model, b the combination of both subevents, c subevent 1, and d subevent 2. The faults are represented by black rectanglesBack to article page