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SUBVOLCANIC ZONED GRANITIC PLUTON IN THE BARTON AND WEAVER PENINSULAS, KING GEORGE ISLAND, ANTARCTICA
https://doi.org/10.15094/00002825
https://doi.org/10.15094/0000282584e2aaae-64df-4313-a3db-822021945d13
名前 / ファイル | ライセンス | アクション |
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KJ00002409872 (1.8 MB)
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Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
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公開日 | 1996-09-01 | |||||
タイトル | ||||||
タイトル | SUBVOLCANIC ZONED GRANITIC PLUTON IN THE BARTON AND WEAVER PENINSULAS, KING GEORGE ISLAND, ANTARCTICA | |||||
言語 | ||||||
言語 | eng | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | subvolcanic zoned pluton | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | King George Island | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | accumulation | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | primary granitic magma | |||||
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 | 10.15094/00002825 | |||||
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 | SUBVOLCANIC ZONED GRANITIC PLUTON IN THE BARTON AND WEAVER PENINSULAS, KING GEORGE ISLAND, ANTARCTICA | |||||
著者名よみ |
/
× /× /× / ナガオ, ケイスケ |
|||||
著者名(英) |
LEE, Jong Ik
× LEE, Jong Ik× HWANG, Jeong× KIM, Hyeoncheol× KANG, Cheon Yun× LEE, Mi Jung× NAGAO, Keisuke |
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著者所属(英) | ||||||
en | ||||||
Polar Research Center, Korea Ocean Research & Development Institute | ||||||
著者所属(英) | ||||||
en | ||||||
Polar Research Center, Korea Ocean Research & Development Institute | ||||||
著者所属(英) | ||||||
en | ||||||
Polar Research Center, Korea Ocean Research & Development Institute | ||||||
著者所属(英) | ||||||
en | ||||||
Polar Research Center, Korea Ocean Research & Development Institute | ||||||
著者所属(英) | ||||||
en | ||||||
Department of Earth Sciences, Seoul National University | ||||||
著者所属(英) | ||||||
en | ||||||
Institute for Study of the Earth's Interior, Okayama University | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | The subvolcanic granitic pluton in the Barton and Weaver Peninsulas, King George Island, is mainly composed of granodiorite with small volumes of gabbro, diorite and aplitic dikes. The pluton shows a vertically compositional zonation; the lower part consists of gabbro and diorite, whereas the upper part is mainly granodiorite. Various geochemical signatures of the pluton confirm that all subunits of the pluton were formed by accumulation and fractionation in a calc-alkaline magma at a shallow level of the crust. The positive Sr and Eu anomalies as well as textural features of gabbro strongly support that gabbro was the cumulate derived from accumulation of calcic plagioclase and in situ crystallization of ferromagnesian minerals. Taking into account the geochemical features of gabbro as a cumulate, the primary magma of the pluton is considered to have been intermediate (dioritic or quartz dioritic) in composition. | |||||
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 9, p. 76-90, 発行日 1996-09 |
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出版者 | ||||||
出版者 | National Institute of Polar Research |