Fig. 9From: Magmatic–hydrothermal system of Aso Volcano, Japan, inferred from electrical resistivity structuresComparison between the cross-sections of S-wave velocity (Huang et al. 2018; contours in each section) and resistivity of our final model (colors in each section) along lines a–d on the topographic map. L and H indicate low- and high-velocity anomalies marked by Huang et al. (2018), respectively. The depth is relative to BSL. The color scale for topography is as in Fig. 1Back to article page