北海道森地熱貯留層におけるCaに富むブライン及びCO2に富む流体の生成:流体包有物のマイクロサーモメトリーによる証拠
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概要
- 論文の詳細を見る
- Society of Resource Geologyの論文
- 1999-03-20
著者
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村松 容一
Department Of Liberal Arts Faculty Of Science And Technology Science University Of Tokyo
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小松 亮
Exploration Department, JMC Geothermal Engineering Co., Ltd.
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MURAMATSU Yoichi
Science University of Tokyo
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KOMATSU Ryo
Japan Metals and Chemicals Co., Ltd.
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Komatsu Ryo
Japan Metals And Chemicals Co. Ltd.
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MURAMATSU Yoichi
Department of Liberal Arts, Faculty of Science and Technology, Science University of Tokyo
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KOMATSU Ryo
Exploration Detartment, JMC Geothermal Engineering Co., Ltd.
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Muramatsu Yoichi
Department Of Liberal Arts Faculty Of Science And Technology Tokyo University Of Science
関連論文
- Prehnite as an indicator of productive fractures in the shallow reservoir, Kakkonda geothermal system, northeast Japan
- 北海道森地熱貯留層に産する流体包有物のガス組成
- 葛根田地熱系に産する脈硬石膏の地化学的特徴
- Geochemical study of fluid inclusions in anhydrite from the Kakkonda geothermal system, northeast Japan
- 北海道森地熱貯留層におけるCaに富むブライン及びCO2に富む流体の生成:流体包有物のマイクロサーモメトリーによる証拠
- Hydrochemistry of the groundwaters in the Izu collision zone and its adjacent eastern area, central Japan
- Hydrochemistry and isotopic characteristics of non-volcanic hot springs around the Miocene Kofu granitic complex surrounding the Kofu Basin in the South Fossa Magna region, central Honshu, Japan