Fig. 5From: Seismotectonics in the Tanzawa Mountains area in the Izu-Honshu collision zone of central Japan, as revealed by precisely determined hypocenters and focal mechanismsKagan angles between the focal mechanisms of earthquakes in depth sections A–B, C–D, and E-F and Reference mechanisms A and B are shown in (a)–(c) and (d)–(f), respectively. The colors indicate the values of the Kagan angle for each focal mechanism. Gray circles indicate earthquakes having focal mechanisms that could not be successfully determined.Back to article page