Fig. 4From: Estimation of shallow S-wave velocity structure using microtremor array exploration at temporary strong motion observation stations for aftershocks of the 2016 Kumamoto earthquakeS-wave velocity profiles estimated from the inversion of the phase velocity in Mashiki (a–c), Aso and Minamiaso (d), Kumamoto (e) and Nishihara (f). The line labeled “KMMH16” represents the results for the model obtained from the borehole logs at the station KMMH16Back to article page