Fig. 3From: Estimate of the contraction rate of central Japan through the deformation of the Philippine Sea slabThe same as Fig. 2, but the Hirose model (Hirose et al. 2008a) is used for the configuration of the PHS slab. The following results are also used for the plate configuration model: Baba et al. (2002), Nakajima and Hasegawa (2007), Hirose et al. (2008b), and Nakajima et al. (2009)Back to article page