Fig. 2From: Source rupture processes of the foreshock and mainshock in the 2016 Kumamoto earthquake sequence estimated from the kinematic waveform inversion of strong motion dataAftershocks larger than JMA magnitude of 2 in four different periods and fault models. Size and color of circles correspond to magnitude and depth of aftershocks. Rectangles represent surface projection of assumed source fault planes of foreshock and mainshock in inversion analysesBack to article page