Metastable corundum + quartz + andalusite association in pelitic granulite from the Kerala Khondalite Belt, southern India
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概要
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Corundum in direct contact with quartz and associated with andalusite has been found as an inclusion in alkali feldspar obtained from a leucosome, which forms a part of migmatized pelitic granulite from the Kerala Khondalite Belt, southern India. Thermodynamically, corundum + quartz is metastable relative to andalusite. Textural features suggest that it is a rare example of an arrested reaction corundum + quartz → andalusite which may have been triggered off by the introduction of H2O-rich fluids along the cracks of the host alkali feldspar during the uplift and cooling of the leucosome. The metastable corundum + quartz association most likely originated during the crystallization of the Al2O3-rich leucosome melt when early corundum came into contact with later quartz under conditions with a relatively low H2O activity.
- 2011-08-01
著者
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Satish-kumar M.
Department Of Biology And Geosciences Faculty Of Science Shizuoka University
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Satish-kumar M.
Inst. Of Geosciences Shizuoka Univ.
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Hokada Tomokazu
National Inst. Polar Res. Tokyo Jpn
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Hokada Tomokazu
National Inst. Of Polar Res.
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KATO Mutsumi
Department of Earth Sciences, Graduate School of Sciences, Chiba University
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Kato Mutsumi
Department Of Earth Sciences Graduate School Of Sciences Chiba University
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Hiroi Yoshikuni
Department Of Earth Sciences Chiba University
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Hiroi Yoshikuni
Dep. Of Earth Sciences Graduate School Of Sciences Chiba Univ.
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Hiroi Yoshikuni
Department Of Earth Sciences Graduate School Of Sciences Chiba University
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HARLOV Daniel
GeoForschungsZentrum Potsdam
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