Fig. 4From: Spatio-temporal characteristics of frictional properties on the subducting Pacific Plate off the east of Tohoku district, Japan estimated from stress drops of small earthquakesSpatially smoothed stress drop derived from (a) P-wave and (b) S-wave analyses, the same as Fig. 3. Thin contours show coseismic displacements of the following M7-8 large earthquakes for the 1968 Tokachi-oki, the 1978 Miyagi-oki, the 1981 Miyagi-oki, the 1989 Sanriku-oki, and the 2003 Miyagi-oki at an interval of 0.5 m (Nagai et al. 2001; Yamanaka and Kikuchi 2004). Areas A and B, corresponding to areas where repeating earthquakes have been observed (Uchida et al. 2007; Okuda and Ide 2018), have higher values of stress drop. Refer to the text in detailBack to article page