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| | Abstract | | In order to investigate a relationship between a distribution of an anamorphic zone and a geophysical imaging in Owakidani geothermal field of Hakone volcano, central Japan, we carried out an electrical resistivity and seismic refraction experiment in same 2 explosion lines with about 100m length. In this session, we describe obtained some cross section results about 30m depth under surface of resistivity/seismic velocity. |
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