Figure 3. Interpolated slip (dots) and derived initial stress vector (thick lines) for the Hyogo-ken Nanbu earthquake in the Yoshida et al. (1996) slip model. Dots show the dislocation of the NW side of the fault at time increments of 0.125 s for each subfault. At subfaults where no initial stress vector is shown, the motions did not specify a unique initial stress. A few subfaults are numbered. Diamonds indicate more reliable stresses. a) Nojima fault. b) Rokko fault system.