Geanulite-facies rocks in several islands west of Langhovde, East Antarctica
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- Katsushima Takayoshi
- Department of Geology and Mineralogy, Faculty of Science, Hokkaido University
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説明
Several islands in the west of Langhovde (69°08′-69°17′S, 39°24′-39°36′E), East Antarctica, are underlain by granulite-facies metamorphic rocks. Among them pyroxene gneiss is the most dominant rock type. It includes garnet-bearing layers, in which orthopyroxene, clinopyroxene, garnet and hornblende are present in equilibrium. These minerals are generally rich in Fe, reflecting the bulk chemistry of the host rocks. Especially, the orthopyroxenes in two specimens of pyroxene gneiss have Fe/(Fe+Mn+Mg) ratios higher than 0.9. The stability field of such Fe-rich orthopyroxenes has been estimated to be more than 9kb at 800℃. On the other hand, the calculated results by the geothermometers using orthopyroxene-clinopyroxene and garnet-clinopyroxene pairs and the geobarometers using a garnet-orthopyroxene-plagioclase association range 750-800℃ and 7-8kb.
収録刊行物
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- Memoirs of National Institute of Polar Research. Special issue
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Memoirs of National Institute of Polar Research. Special issue 37 95-110, 1985-09
国立極地研究所
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詳細情報 詳細情報について
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- CRID
- 1570572701838482432
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- NII論文ID
- 110000010026
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- NII書誌ID
- AA00733561
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- ISSN
- 03860744
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- 本文言語コード
- en
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- データソース種別
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- CiNii Articles