
| ID | 13878 |
| Eprint ID | 13878
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| フルテキストURL | |
| 著者 |
Saieev K
Graduate school of Natural science and Technology, Okayama University
小山内 康人
岡山大学教育学部地学教室
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| 抄録 | The geology of Ganguvapatti area situated at the central Madurai block of southern India consisting of varous high-grade metamorphic rock types. This contribution briefly describes the geology, field occurrences and petrography of metamorphic rock from Ganguvarpatti area. Ganguvarpatti is known for its occurrence of sapphirine-bearing UHT granulites while the surrounding granulites are less studied. So in this contribution we have discussed the pressure-temperature stability and evolution of granulites surrounding UHT granulites. The pressure-temperature estimation of garnet-orthopyroxene-cordierite granulite resulted a near peak temperature condition of>950゜ C at a pressure between 9-10 kbar. These results are in good agreement with the stability field in the KFMASH petrogenetic frid.
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| キーワード | Madurai block
southrn India
UHT-granulites
P-T estimation
multi-stage evolution
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| 発行日 | 2002-09-20
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| 出版物タイトル |
Okayama University Earth Science Report
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| 出版物タイトル(別表記) | 岡山大学地球科学研究報告
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| 巻 | 9巻
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| 号 | 1号
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| 出版者 | 岡山大学理学部地球科学教室
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| 出版者(別表記) | Department of Earth Sciences Faculty of Science, Okayama University
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| 開始ページ | 1
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| 終了ページ | 8
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| ISSN | 1340-7414
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| NCID | AN10506284
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| 資料タイプ |
紀要論文
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| 言語 |
英語
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| 著作権者 | 岡山大学地球科学研究報告編集委員会
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| 論文のバージョン | publisher
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| 査読 |
無し
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| Eprints Journal Name | esr
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