Fig. 11.From: Seismicity and crustal structure in the vicinity of the southern Itoigawa-Shizuoka Tectonic LineHypocenter distribution near the southern segments of the ISTL fault system after the DD tomography relocation. White circles: relocated events. Black diamonds: location determined by the Japanese Meteorological Agency (JMA). White connecting line: shift in the epicentral location and hypocentral depth. The events were relocated an average of 2 km shallower than the JMA position.Back to article page