Fig. 7
From: 2D resistivity model around the rupture area of the 2011 Tohoku-oki earthquake (Mw 9.0)
a Coseismic slip distribution below the OBEM survey line during the 2011 Tohoku-oki earthquake (Iinuma et al. 2012). b The optimal resistivity model (Model III) with interpretation. Thick and thin dashed lines denote the backstop fault and the bottom of the subseafloor sediment layer based on a seismic survey at line TH03 (Kodaira et al. 2017), respectively. The horizontal and vertical scale ratio of images is 1:2