Fig. 2From: Applicability of source scaling relations for crustal earthquakes to estimation of the ground motions of the 2016 Kumamoto earthquakeRelationship between rupture area and seismic moment for crustal earthquakes. Two broken green lines indicate one SD (σ = 0.14) for inland crustal earthquakes in Japan. The large red triangle represents the logarithmic average of the rupture areas of the three models for the 2016 Kumamoto earthquake (M w 7.0) shown in Table 1. The small red triangles indicate the rupture areas from individual modelsBack to article page