Fig. 5.From: Rate/state Coulomb stress transfer model for the CSEP Japan seismicity forecastSpatial summation of ΔCFF caused by the large earthquakes since 1891, listed in Table 1 and shown in Fig. 3. Stresses are resolved on two assumed nodal planes (Fig. 4(b)) and the maximum values through the seismogenic depth of 5–15 km are chosen. Dashed line indicates plate boundary.Back to article page