Manganoan winchite in a quartz schist from the Saruta-gawa area in the Sanbagawa metamorphic terrain, central Shikoku, Japan.
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- BANNO Yasuyuki
- Geological Museum, Geological Survey of Japan
Bibliographic Information
- Other Title
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- 四国中央部三波川帯猿田川地域の石英片岩中に産する含Mnウインチ閃石
- Manganoan winchite in a quartz schist f
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Abstract
Manganoan winchite (up to 4.19 wt.% MnO) occurs as cores of zoned amphibole in a quartz schist from the Saruta-gawa area in the Sanbagawa metamorphic terrain, central Shikoku, Japan. The quartz schist consists of quartz, albite, amphibole, muscovite, garnet, chlorite, allanite, calcite, apatite, stilpnomelane, tourmaline, hematite and pyrite. The amphibole is euhedral to subhedral in form (up to 700 μm long). The core of the amphibole ranges in composition from barroisite through winchite to manganoan winchite. The amphibole is rimmed by alkali amphibole (mainly magnesioriebeckite) and winchite. Garnet in the quartz schist is rich in spessartine component (59-79%).
Journal
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- JOURNAL OF MINERALOGY, PETROLOGY AND ECONOMIC GEOLOGY
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JOURNAL OF MINERALOGY, PETROLOGY AND ECONOMIC GEOLOGY 92 (5), 189-194, 1997
Japan Association of Mineralogical Sciences
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Details 詳細情報について
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- CRID
- 1390282681210617088
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- NII Article ID
- 10002088862
- 30022306511
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- NII Book ID
- AN10047992
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- COI
- 1:CAS:528:DyaK2sXltlektbs%3D
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- ISSN
- 18813275
- 09149783
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- NDL BIB ID
- 4265976
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- Text Lang
- en
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- Data Source
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- JaLC
- NDL
- Crossref
- CiNii Articles
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- Abstract License Flag
- Disallowed