Fig. 11

Comparison of the coseismic slip distribution of the Genroku event with the interseismic slip-deficit rate distribution. The blue and red scale contours represent the interseismic slip-deficit and slip-excess rate distribution, respectively, estimated from GPS data (Noda et al. 2013). The superposed yellow green contours at the interval of 4 m represent the coseismic slip distribution of the 1703 Genroku event in Fig. 5a. The total rupture area of the Taisho and Genroku events (Fig. 10) almost agrees with the interseismic slip-deficit area extending along the Sagami trough except the Izu-Mainland collision zone. The thin solid curves are the isodepth contours of the upper boundary surface for the descending Philippine Sea plate