Fig. 1From: Evaluating variability in coseismic slips of paleoearthquakes from an incomplete slip history: an example from displaced terrace flights across the Kamishiro fault, central JapanActive fault map around the ISTL active fault system. a Active faults in central Japan and the ISTL composing of three major segments, each separated by change in slip direction and surface geometry of the fault trace (Nakata and Imaizumi, 2002). b The 2014 surface rupture, denoted as blue lines, occurred on approximately one-third of the previously known Kamishiro fault. The trench sites correspond with those in Fig. 10. The Otari–Nakayama fault is from Kato et al. (1989) and Nakano et al. (2002). ISTL Itoigawa–Shizuoka Tectonic Line, JMA Japan Meteorological AgencyBack to article page