Fig. 3From: Seismic velocity structure at the southern termination of the 2016 Kumamoto Earthquake rupture, JapanInitial and final velocity models in this study. Solid lines = initial 1-D models used for the tomography, based on JMA2001 (Ueno et al. 2002). Dotted lines = tentative 1-D models used to determine the initial hypocenter locations. Diamonds = mean velocity in each depth layer that was acquired by the tomographic inversionBack to article page