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Br/Cl ratios and trace element analysis of fluid inclusions from the Tsushima granite.
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- Kurosawa Masanori
- Life Env. Sci., Univ. Tsukuba
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- Shin Ki-Cheol
- Res. Inst. Hum. Nat.
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- Sasa Kimikazu
- Pure Appl. Sci., Univ. Tsukuba
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- Ishii Satoshi
- Res. Fac. C., Univ. Tsukuba
Bibliographic Information
- Other Title
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- 流体包有物のBr/Cl比から見た対馬花崗岩の流体形成
Description
Br and Cl ratios and trace-element contents of fluid inclusions in quartz from miarolitic cavities and quartz veins at the Tsushima granite, Nagasaki Pref., Japan, were analyzed by particle-induced X-ray emission (PIXE) to examine chemistries of granite-derived fluids in granite body with shallow emplacement level. Two-phase fluid inclusions from the cavities and quartz veins in the body and the surrounding Pb-Zn ore deposit have Br/Cl weight ratios of about 0.0010. Polyphase inclusions from the cavities and the quartz veins in the body yield Br/Cl ratios of about 0.0030, while those from quartz veins in the ore deposit range from 0.0074 to 0.0120.
Journal
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- Abstracts for Annual Meeting of Japan Association of Mineralogical Sciences
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Abstracts for Annual Meeting of Japan Association of Mineralogical Sciences 2010 (0), 81-81, 2010
Japan Association of Mineralogical Sciences
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Keywords
Details 詳細情報について
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- CRID
- 1390001205544743936
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- NII Article ID
- 130004601730
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- Text Lang
- ja
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- Data Source
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- JaLC
- CiNii Articles
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- Abstract License Flag
- Disallowed