Magnetotelluric survey and three-dimensional resistivity structure in and around the Niseko area, southwestern Hokkaido

被引:4
|
作者
Tamura, Makoto [1 ,7 ]
Oka, Daisuke [1 ]
Okazaki, Noritoshi [1 ]
Suzuki, Koichi [2 ,3 ]
Hashimoto, Takeshi [4 ]
Mogi, Toru [5 ,6 ]
机构
[1] Hokkaido Res Org, Res Inst Energy Environm & Geol, Sapporo, Japan
[2] Hokkaido Univ, Fac Engn, Sapporo, Japan
[3] Kawasaki Geol Engn Co Ltd, Tokyo, Japan
[4] Hokkaido Univ, Inst Seismol & Volcanol, Fac Sci, Sapporo, Japan
[5] Tokyo Inst Technol, Volcan Fluid Res Ctr, Tokyo, Japan
[6] Nagoya Univ, Earthquake & Volcano Res Ctr, Nagoya, Japan
[7] Kita19 Jo Nishi12 Chome,Kita Ku, Sapporo, Hokkaido 0600819, Japan
关键词
Supercritical geothermal fluids; Niseko volcanic group; Magnetotelluric observation; Resistivity structure; Sub-vertical conductor; GEOTHERMAL SYSTEMS; INVERSION;
D O I
10.1016/j.geothermics.2022.102496
中图分类号
TE [石油、天然气工业]; TK [能源与动力工程];
学科分类号
0807 ; 0820 ;
摘要
Supercritical geothermal systems (SGS) have the potential to drastically increase geothermal power generation. The New Energy and Industrial Technology Development Organization (NEDO, Japan) has recently started to research and develop supercritical geothermal power generation. Our team conducted a field survey and data collection at three areas in Japan, to characterize the SGS and evaluate the potential for supercritical geothermal power generation. Here, we present a three-dimensional resistivity structure by observing 112 magnetotelluric and 4 telluric sites in and around the Niseko area, southwestern Hokkaido. The final resistivity structure showed a dominant sub-vertical conductor beneath the central part of the Niseko volcanic group. We inferred that the supercritical geothermal fluids possibly exist below an altitude of about-3 km inside or edge of the conductor.
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收藏
页数:18
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