花崗岩質マグマと共存する流体:岩手県宮古花崗岩および山口Cu-W鉱床に産する含灰重石アプライト脈中のREEとCuの地球化学的特徴 Coexistence of a Fluid Phase with Granitic Magma: Geochemical Characteristics of REE and Cu in Miyako Granite and in Scheelite-bearing Aplitic Veins at the Yamaguchi Cu-W Skarn Deposit, Iwate, Japan
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- 緒方 武幸 OGATA Takeyuki
- Department of Earth Science and Technology, Faculty of Engineering and Resources Science, Akita University
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- 石山 大三 ISHIYAMA Daizo
- Department of Earth Science and Technology, Faculty of Engineering and Resources Science, Akita University
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- 水田 敏夫 [他] MIZUTA Toshio
- Department of Earth Science and Technology, Faculty of Engineering and Resources Science, Akita University
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- NAKASHIMA Kazuo
- Department of Earth Science, Faculty of Science, Yamagata University
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Author(s)
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- 緒方 武幸 OGATA Takeyuki
- Department of Earth Science and Technology, Faculty of Engineering and Resources Science, Akita University
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- 石山 大三 ISHIYAMA Daizo
- Department of Earth Science and Technology, Faculty of Engineering and Resources Science, Akita University
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- 水田 敏夫 [他] MIZUTA Toshio
- Department of Earth Science and Technology, Faculty of Engineering and Resources Science, Akita University
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- NAKASHIMA Kazuo
- Department of Earth Science, Faculty of Science, Yamagata University
Journal
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- Resource Geology
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Resource Geology 52(2), 173-186, 2002-07-25
Society of Resource Geology
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