Fig. 9From: Deep crustal structure around the Atotsugawa fault system, central Japan: A weak zone below the seismogenic zone and its role in earthquake generationComparison of (a) P- and (b) S-wave velocity distributions at a depth of 25 km obtained in this study with (c) P- and (d) S-wave velocity distributions obtained by Nakajima and Hasegawa (2007a) (NH07). (e) Locations of the Atotsugawa (AGF), Mozumi-Sukenobu (MSF), and Ushikubi (UKF) faults and the NKTZ.Back to article page