Fig. 7From: Seismic potential around the 2018 Hokkaido Eastern Iburi earthquake assessed considering the viscoelastic relaxationTime evolution of ΔCFF(t) at three points along the southern fault (S1–S3 in Fig. 6b) and the point along the SI fault (I1 in Fig. 6c). The solid and dashed lines indicate the cases for η = 1019 Pa s and 1020 Pa s, respectivelyBack to article page