Fig. 12
From: Stress field in northeastern Japan and its relationship with faults of recent earthquakes
Slip tendency (ST) values determined using the stress parameter estimated with the slip instability method. A The ST values with westward-dipping plane. B The ST values with eastward-dipping plane. C The distribution of the target events. The left boxes in A and B show the ST value of the fault model. The color of the nodal planes indicates the ST value. The arrows on the nodal plane denote the dipping directions. The number written at the top of each box indicates the stress field in Fig. 11 used to calculate ST value