WEKO3
アイテム
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ARRESTED CHARNOCKITE FORMATION IN SRI LANKA : FIELD AND PETROGRAPHICAL EVIDENCE FOR LOW-PRESSURE CONDITIONS
https://doi.org/10.15094/00002635
https://doi.org/10.15094/000026359dcfee79-6645-4af3-a732-9f7e4c9a90de
名前 / ファイル | ライセンス | アクション |
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KJ00002368247 (3.2 MB)
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Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
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公開日 | 1990-09-01 | |||||
タイトル | ||||||
タイトル | ARRESTED CHARNOCKITE FORMATION IN SRI LANKA : FIELD AND PETROGRAPHICAL EVIDENCE FOR LOW-PRESSURE CONDITIONS | |||||
言語 | ||||||
言語 | eng | |||||
資源タイプ | ||||||
資源タイプ識別子 | http://purl.org/coar/resource_type/c_6501 | |||||
資源タイプ | departmental bulletin paper | |||||
ID登録 | ||||||
ID登録 | 10.15094/00002635 | |||||
ID登録タイプ | JaLC | |||||
ページ属性 | ||||||
内容記述タイプ | Other | |||||
内容記述 | P(論文) | |||||
論文名よみ | ||||||
その他のタイトル | ARRESTED CHARNOCKITE FORMATION IN SRI LANKA : FIELD AND PETROGRAPHICAL EVIDENCE FOR LOW-PRESSURE CONDITIONS | |||||
著者名よみ |
ヒロイ, ヨシクニ
× ヒロイ, ヨシクニ× アサミ, マサオ× /× / カガミ, ヒロオ× / マツエダ, ヒロハル× モトヨシ, ヨウイチ× オゴ, ヨシエ× オサナイ, ヤスヒト× オワダ, マサアキ× /× / シライシ, カズユキ× / ヨシダ, マサル |
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著者名(英) |
HIROI, Yoshikuni
× HIROI, Yoshikuni× ASAMI, Masao× COORAY, P.G.× FERNANDO, M.R.D.× JAYATILEKE, J.M.S.× KAGAMI, Hiroo× MATHAVAN, V.× MATSUEDA, Hiroharu× MOTOYOSHI, Yoichi× OGO, Yoshie× OSANAI, Yasuhito× OWADA, Masaaki× PERERA, L.R.K.× PRAME, K.B.N.× RANASINGHE, N.S.× SHIRAISHI, Kazuyuki× VITANAGE, P.W.× YOSHIDA, Masaru |
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著者所属(英) | ||||||
en | ||||||
Department of Earth Sciences, Faculty of Science, Chiba University | ||||||
著者所属(英) | ||||||
en | ||||||
Department of Geological Sciences, College of Liberal Arts, Okayama University | ||||||
著者所属(英) | ||||||
en | ||||||
Institute of Fundamental Studies, Hantana Road | ||||||
著者所属(英) | ||||||
en | ||||||
Geological Survey Department, Sri Jinaratana Road | ||||||
著者所属(英) | ||||||
en | ||||||
Ceylon Institute of Scientific and Industrial Research | ||||||
著者所属(英) | ||||||
en | ||||||
Institute for Study of Earth's Interior, Okayama University | ||||||
著者所属(英) | ||||||
en | ||||||
Department of Geology, University of Peradeniya | ||||||
著者所属(英) | ||||||
en | ||||||
Department of Geology and Mineralogy, Faculty of Science, Hokkaido University | ||||||
著者所属(英) | ||||||
en | ||||||
National Institute of Polar Research | ||||||
著者所属(英) | ||||||
en | ||||||
Department of Earth Sciences, Faculty of Science, Chiba University | ||||||
著者所属(英) | ||||||
en | ||||||
Department of Geological Sciences, Fukuoka University of Education | ||||||
著者所属(英) | ||||||
en | ||||||
Department of Geological Sciences, Fukuoka University of Education | ||||||
著者所属(英) | ||||||
en | ||||||
Department of Geology, University of Peradeniya | ||||||
著者所属(英) | ||||||
en | ||||||
Geological Survey Department, Sri Jinaratana Road | ||||||
著者所属(英) | ||||||
en | ||||||
Geological Survey Department, Sri Jinaratana Road | ||||||
著者所属(英) | ||||||
en | ||||||
National Institute of Polar Research | ||||||
著者所属(英) | ||||||
en | ||||||
Department of Geology, University of Peradeniya | ||||||
著者所属(英) | ||||||
en | ||||||
Department of Geosciences, Faculty of Science, Osaka City University | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | Field data of the arrested charnockite (orthopyroxene-bearing quartzo-feldspathic rock in a broad sense) formation are the striking evidence for CO_2 flushing and resultant subsolidus dehydration reactions and/or partial melting. Such a local phenomenon is, however, distinct from the preceding regional granulite-facies metamorphism, because it took place under much lower-pressure conditions in Sri Lanka. The orthopyroxene+cordierite+K-feldspar as well as orthopyroxene+garnet+K-feldspar±cordierite assemblages are stable in the charnockitized pelitic rocks of the Southwestern Group. In addition, secondary andalusite occurs commonly, though small in amount, together with siderite and cordierite in other pelitic rocks (gneiss and migmatite) of the Southwestern Group. Secondary andalusite has also been revealed to occur in the Highland Series rocks. This, along with the occurrence of relict kyanite in sillimanite-stable rocks of both the Highland Series and the Southwestern Group establishes that rocks, at least metasediments, of these geological units in Sri Lanka have similar pressure-temperature histories. The later low-pressure metamorphic overprint including arrested charnockite formation was, however, much more extensive in the Southwestern Group than in the Highland Series. | |||||
雑誌書誌ID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AA1072335X | |||||
書誌情報 |
Proceedings of the NIPR Symposium on Antarctic Geosciences 巻 4, p. 213-230, 発行日 1990-09 |
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出版者 | ||||||
出版者 | National Institute of Polar Research |