Fig. 6From: Seismotectonics in the Tanzawa Mountains area in the Izu-Honshu collision zone of central Japan, as revealed by precisely determined hypocenters and focal mechanismsFrequency distribution of the Kagan angle for earthquakes that occurred in Regions A and B. (a) Reference A, (b) Reference B. The Y axis is normalized by the total number of events in each region.Back to article page