Fig. 9.From: InSAR-derived crustal deformation and fault models of normal faulting earthquake (Mj 7.0) in the Fukushima-Hamadori areaSlip distribution on (a) the Shionohira fault, (b) the Yunotake fault, and (c) the Idosawa fault, inferred from the inversion of the InSAR displacement. The arrows show slip vectors of the hanging wall. The contour interval is 50 cm. The positions of the left and right upper edges for each fault plane are shown in Fig. 8.Back to article page