SUBVOLCANIC ZONED GRANITIC PLUTON IN THE BARTON AND WEAVER PENINSULAS, KING GEORGE ISLAND, ANTARCTICA
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概要
- 論文の詳細を見る
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.
- 国立極地研究所の論文
著者
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Nagao Keisuke
Institute for Study of Earth's Interior, Okayama University
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Lee Mi
Department Of Dermatology Asan Medical Center University Of Ulsan College Of Medicine
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Kim Hyeoncheol
Polar Research Center Korea Ocean Research & Development Institute
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Lee Mi
Korea Institute Of Geoscience & Mineral Resources
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Lee J
Korea Polar Research Institute Kordi
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LEE Jong
Polar Research Center, Korea Ocean Research and Development Institute
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HWANG Jeong
Polar Research Center, Korea Ocean Research & Development Institute
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KANG Cheon
Polar Research Center, Korea Ocean Research & Development Institute
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Kang Cheon
Polar Research Center Korea Ocean Research & Development Institute
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Hwang Jeong
Polar Research Center Korea Ocean Research & Development Institute
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Lee Mi
Department Mathematics Pusan National University
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Lee Jong
Polar Research Center Korea Ocean Research & Development Institute
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Nagao Keisuke
Institute For Study Of Earth's Interior Okayama University
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NAGAO Keisuke
Institute for Study of the Earth's Interior, Okayama University
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