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Progress in Earth and Planetary Science
Figure 7 | Progress in Earth and Planetary Science

Figure 7

From: Hydrothermal system in the Tatun Volcano Group, northern Taiwan, inferred from crustal resistivity structure by audio-magnetotellurics

Figure 7

Comparison between inverted results and in-situ measurement. (a) Resistivities along borehole E203, shown in Figure 6. Red and black lines represent the resistivities obtained by this study and by well logging (MRSO [1970]), respectively. (b) Geologic section along sites 102, 005, 006, and 007 at the foot of Mt. Chishinshan (MRSO [1973]). Red lines represent the isotherm obtained from temperature logging of the boreholes (MRSO [1973]). The locations of the boreholes are shown by the squares in Figure 1.

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