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公開日 : 2002-05-18
8.01 MB
著者
阪本 志津枝
内容記述(抄録等)
The Osayama ultramafic body occurs in the high-P/T Sangun metamorphic belt, southwest Japan. The northeastern parts of the Osayama ultramafic body are a serpentinite melange with tectonic blocks of diverse lithology and metamorphic grade. Chemical compositions of the constituent minrals from the tectonic blocks such as kosmochlor-bearing and -free actinolite-tremolite rocks and jadeitites in the Osayama ultramafic body are provided in this paper.

掲載誌情報
島根大学総合理工学部紀要. シリーズA 31 , 217 - 241 , 1997-12-26
出版者
島根大学総合理工学部
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