Carbonaceous matter in quartz veins and pelitic rocks from the Ryoke metamorphic belt in the Yanai district, SW Japan
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概要
- 論文の詳細を見る
Carbonaceous matter (CM) with various modes of occurrence has been observed in quartz veins in the biotite zone of the Ryoke metamorphic belt in the Yanai district, Yamaguchi Prefecture, SW Japan. Raman spectroscopic analysis of the CM revealed that high temperature fluids had percolated through fractures, which were now occupied by the quartz veins that had formed during the retrograde stages of metamorphism. These fluids may have also affected the degree of organization of the fine-grained CM particles in the host pelitic rocks and the coarse-grained particles that had precipitated from them at a later stage.
- 日本鉱物科学会の論文
- 2007-10-01
著者
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星野 健一
広島大 理
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Hoshino Kenichi
Dep. Of Earth And Planetary Systems Sci. Hiroshima Univ.
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Hoshino K
Department Of Earth And Planetary Sciences Hiroshima University
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Hoshino Kenichi
Dep. Of Earth And Planetary Systems Sci. Graduate School Of Sci. Hiroshima Univ.
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Hoshino Kenichi
Department Of Earth And Planetary Sciences Hiroshima University
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Hoshino Kenichi
Department Of Earth And Planetary Systems Science Graduate School Of Science Hiroshima University
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HIROTAKA Tomoe
Department of Earth and Planetary Systems Science, Hiroshima University
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Hirotaka Tomoe
Department Of Earth And Planetary Systems Science Hiroshima University
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