Ultrahigh temperature sapphirine-osumilite and sapphirine-quartz granulites from Bunt Island in the Napier Complex, East Antarctica -Reconnaissance estimation of P-T evolution -
スポンサーリンク
概要
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The summer party of the 39th Japanese Antarctic Research Expedition (1997-1998) carried out geological field work on Bunt Island at the southeastern end of Amundsen Bay, Enderby Land, which is in the highest-grade metamorphic region in the Napier Complex. The island is underlain by various kinds of ultrahigh-temperature (UHT) metamorphic rocks including osumilite-bearing aluminous sapphirine-garnet-orthopyroxene granulite and quartz-predominant sapphirine-garnet-sillimanite gneiss containing the assemblage sapphirine-quartz. Osumilite-bearing aluminous granulite is silica-undersaturated, aluminous and magnesian chromium-rich chemical affinity. Osumilite-bearing granulite from Bunt Island could be formed through the mixing of clayey materials or other felsic components derived from felsic igneous rocks with a relatively high proportion of mafic to ultramafic detritus in the sedimentary precursor. The chemical mixing could have taken place during c. 3.2 and c. 2.5 Ga. P-T estimation for osumilite-bearing granulite and related sapphirine-quartz gneiss indicates ultrahigh-temperature condition (〜1100℃, 〜1100 Mpa) as well as other high-grade rocks from the Napier Complex, but the rocks from Bunt Island clearly show isothermal decompression in part of the clockwise P-T evolutional process.
- 国立極地研究所の論文
著者
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Hokada Tomokazu
National Institute of Polar Research, 10-3 Midori-cho, Tachikawa, Tokyo 190-8518, Japan
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KUSACHI Isao
Department of Earth Sciences, Faculty of Education, Okayama University
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Kusachi I
Okayama Univ. Okayama Jpn
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Kusachi Isao
Dep. Of Earth Sciences Fac. Of Education Okayama Univ.
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Kusachi Isao
Department Of Earth Sciences Okayama University
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Kusachi Isao
Department Of Earth Science Faculty Of Education Okayama University
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Osanai Yasuhito
Department of earth sciences, Okayama university
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Kusachi Isao
Department Of Earth Sciences Faculty Of Education Okayama Univresity
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OWADA Masaaki
Department of Earth Sciences, Yamaguchi University
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TSUNOGAE Toshiaki
Institute of Geoscience, University of Tsukuba
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TOYOSHIMA Tsuyoshi
Department of Earth Sciences, Niigata University
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Osanai Yasuhito
Division Of Evolution Of Earth Environments Faculty Of Social Andcultural Studies Kyushu University
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Osanai Y
Fukuoka Univ. Education Munakata Jpn
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Osanai Yasuhito
Department Of Earth And Planetary System Science Okayama University
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Osanai Yasuhito
Division Of Evolution Of Earth Environments Kyushu University
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Hokada Tomokazu
National Institute Of Polar Research 10-3 Midori-cho Tachikawa Tokyo 190-8518 Japan
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Crowe Warwick
Department of Geology and Geophysics, University of Western Australia
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Crowe Warwick
Department Of Geology And Geophysics University Of Western Australia
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Osanai Yasuhito
Division Of Evolution Of Earth Environments Faculty Of Social And Cultural Studies Kyushu University
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Tsunogae Toshiaki
Graduate School Of Science And Technology Niigata University
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Tsunogae Toshiaki
Institute Of Geoscience The University Of Tsukuba
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Owada Masaaki
Division Of Earth Sciences Graduate School Of Science And Technology Yamaguchi University
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Owada Masaaki
Department Of Earth Sciences University Of Yamaguchi
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Hamamoto T
Dia Consultants Co. Ltd. Aichi Jpn
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Hamamoto Takuji
Graduate School Of Science And Technology Niigata University
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Osanai Y
Division Of Evolution Of Earth Environments Faculty Of Social And Cultural Studies Kyushu University
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Crowe Warwicka.
Department Of Geology And Geophysics University Of Western Australia
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Osanai Y
Division Of Earth Sciences Faculty Of Social And Cultural Studies Kyushu University
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Owada Masaaki
Department Of Mineral Science And Geology Faculty Of Science Yamaguchi University
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Osanai Yasuhito
Division Of Earth Sciences Faculty Of Social And Cultural Studies Kyushu University
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Hokada Tomokazu
National Inst. Of Polar Res.
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Tsunogae T
Univ. Tsukuba Ibraki Jpn
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