Fig. 7
From: Magmatic–hydrothermal system of Aso Volcano, Japan, inferred from electrical resistivity structures
Comparison of the resistivity cross-sections of Takakura et al. (2000; upper diagrams of a, b) and those of the present study (lower diagrams of a, b). The sections in a are along the NNE–SSW-oriented line A–A’ in c, and the sections in b are along the NNE–SSW-oriented line B–B’ in c. c Topographic map. Closed squares in c and arrows in a, b indicate the locations of wells W1 and W2. The vertical exaggeration is ×2. The depth values are BSL