Fig. 4From: 2D resistivity model around the rupture area of the 2011 Tohoku-oki earthquake (Mw 9.0)Sounding curves at sites 30, 23, and 41. Dots with error bars show observed data. Error bars include the error floor (see text). The dashed and solid lines are the responses predicted by the initial model used for the inversion (Model 0) and the optimal model (Model III), respectivelyBack to article page