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Fig. 5 | Progress in Earth and Planetary Science

Fig. 5

From: Spatial pattern in stress drops of moderate-sized earthquakes on the Pacific Plate off the south-east of Hokkaido, Japan: implications for the heterogeneity of frictional properties

Fig. 5

Magnified images of the three coseismic source areas shown in Fig. 4d for a the 1968 Tokachi-oki (Nagai et al. 2001), b 2003 Tokachi-oki (Yamanaka and Kikuchi 2003), and c 1973 Nemuro-oki earthquakes (Yamanaka 2006). The interval of the coseismic slip is 1 m (as in Fig. 4). The dominant area of the afterslip following the 2003 Tokachi-oki earthquake is indicated by a broken blue line. Please refer to Miyazaki et al. (2004, 2004) for details

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