Fig. 2From: Estimation of shallow S-wave velocity structure using microtremor array exploration at temporary strong motion observation stations for aftershocks of the 2016 Kumamoto earthquakePhase velocity dispersion curves in Mashiki (a–c), Aso and Minamiaso (d), Kumamoto (e) and Nishihara (f). The gray line in (a) shows the calculation results for the model obtained at KMMH16 from borehole logs. In each plot, warm and cool colors correspond to sites experiencing heavy and light damage, respectivelyBack to article page