Fig. 7.From: Deep structure of the Ou mountain range strain concentration zone and the focal area of the 2008 Iwate-Miyagi Nairiku earthquake, NE Japan—seismogenesis related with magma and crustal fluid(a) Vp perturbation at a depth of 24 km. (b) Vp /Vs distribution at a depth of 24 km. Other Vp /Vs distributions are the same as in Fig. 6(b).Back to article page