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Fig. 10. | Earth, Planets and Space

Fig. 10.

From: InSAR-derived crustal deformation and fault models of normal faulting earthquake (Mj 7.0) in the Fukushima-Hamadori area

Fig. 10.

Residual distribution as a function of dip angle of the Yunotake fault. The vertical axis indicates the normalized residual to be 0 to 1. On each panel, the dip angle of the Shionohira fault is fixed at a certain angle indicated at the upper left. Individual lines on each panel are the residuals of when the dip angle of the Idowasa fault is fixed at a certain angle. The characters “W” and “E” mean west-dipping and east-dipping for the Idosawa fault, respectively.

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