Gernet-sillimanite gneisses from the Lutzow-Holm Bay region East Antarctica
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概要
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This paper presents the regional distribution and petrographical features of garnet-sillimanite gneisses in the Lutzow-Holm Bay region, East Antarctica. In addition to sillimanite, such aluminous silicate and oxide minerals as kyanite, staurolite, sapphirine and spinel occur in the gneisses. Among them, sapphirine is the first report in a pelitic rock from the region. From their microscopic textures, it is inferred that the rocks in the region suffered the prograde metamorphism of kyanite-sillimanite type as those in the Prince Olav Coast did. Thus, it is clarified that the rocks in the present region and the Prince Olav Coast have the same metamorphic history and possibly belong to the same geological unit. The metamorphic grade is expected to increase progressively towards the southern part of the Lutzow-Holm Bay region.
- 国立極地研究所の論文
著者
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MATSUMOTO Yukio
Department of Preventive Medicine and Public Health, School of Medicine, Keio University
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Motoyoshi Y
National Inst. Polar Res. Tokyo Jpn
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Motoyoshi Yoichi
Department Of Geology And Mineralogy Faculty Of Science Hokkaidouniversity
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Motoyoshi Yoichi
Department Of Applied Geology University Of New South Wales:(present Address)national Institute Of P
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MATSUEDA Hiroharu
Institute of Mining Geology, Mining College, Akita University
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Matsubara Satoshi
National Science Museum
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Matsueda Hiroharu
Institute Of Mining College Akita University
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Matsubara S
National Science Museum
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Matsumoto Yukio
Department Of Geology Faculty Of Liberal Arts Nagasaki University
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Matsumoto Yukio
Department Of Anesthesiology Fukushima Medical University School Of Medicine
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Matsumoto Yukio
Department of Mineralogical Sciences and Geology, Faculty of Science, Yamaguchi University
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