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CORUNDUM+QUARTZ ASSOCIATION IN ARCHEAN GRANULITE-FACIES ROCK FROM ENDERBY LAND, EAST ANTARCTICA : PRELIMINARY INTERPRETATION
https://doi.org/10.15094/00002536
https://doi.org/10.15094/00002536b6bd7bba-142f-44af-8e47-ce7dbb478822
名前 / ファイル | ライセンス | アクション |
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KJ00002368073 (866.1 kB)
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Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
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公開日 | 1987-09-01 | |||||
タイトル | ||||||
タイトル | CORUNDUM+QUARTZ ASSOCIATION IN ARCHEAN GRANULITE-FACIES ROCK FROM ENDERBY LAND, EAST ANTARCTICA : PRELIMINARY INTERPRETATION | |||||
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 | 10.15094/00002536 | |||||
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 | CORUNDUM+QUARTZ ASSOCIATION IN ARCHEAN GRANULITE-FACIES ROCK FROM ENDERBY LAND, EAST ANTARCTICA : PRELIMINARY INTERPRETATION | |||||
著者名よみ |
モトヨシ, ヨウイチ
× モトヨシ, ヨウイチ× マツエダ, ヒロハル |
|||||
著者名(英) |
MOTOYOSHI, Yoichi
× MOTOYOSHI, Yoichi× MATSUEDA, Hiroharu |
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著者所属(英) | ||||||
en | ||||||
Department of Geology and Mineralogy, Faculty of Science, Hokkaido University:(Present address)Department of Applied Geology, University of New South Wales | ||||||
著者所属(英) | ||||||
en | ||||||
Institute of Mining Geology, Mining College, Akita University | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | Corundum occurs in direct contact with quartz in a high-temperature granulite-facies metamorphosed quartzite from the Archean Napier Complex in Enderby Land, East Antarctica. The quartzite is composed dominantly of bluish-gray quartz with mesoperthitic K-feldspar and spinel as subordinate constituents. Corundum occurs always being interlocked with spinel and both minerals are in direct contact with quartz. Under the P-T conditions of the Napier granulites (900-1000℃, 7-10kbar), sillimanite should be a stable Al_2SiO_5,and corundum cannot coexist stably with quartz. On the basis of the petrographical evidence, the corundum is inferred to be an exsolved product from spinel solid solution upon cooling, and it did not react with surrounding quartz to form Al_2SiO_5 probably due to the high activation energy required for the solid-solid interaction between corundum and quartz. | |||||
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 1, p. 107-112, 発行日 1987-09 |
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出版者 | ||||||
出版者 | National Institute of Polar Research |