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  1. 紀要論文
  2. 琉球大学教育学部紀要
  3. 92号
  1. 部局別インデックス
  2. 教育学部

東南極セール・ロンダーネ山地,ブッラットニーパネの崖錐に含まれる塩基性グラニュライトの変成組織

http://hdl.handle.net/20.500.12000/39207
http://hdl.handle.net/20.500.12000/39207
c133633a-4d3b-4704-9654-868b571bd456
名前 / ファイル ライセンス アクション
no92p161.pdf no92p161.pdf
Item type デフォルトアイテムタイプ(フル)(1)
公開日 2018-04-11
タイトル
タイトル 東南極セール・ロンダーネ山地,ブッラットニーパネの崖錐に含まれる塩基性グラニュライトの変成組織
言語 ja
作成者 Baba, Sotaro

× Baba, Sotaro

en Baba, Sotaro

Uesato, Moeko

× Uesato, Moeko

en Uesato, Moeko

Hokada, Tomokazu

× Hokada, Tomokazu

en Hokada, Tomokazu

Adachi, Tatsuro

× Adachi, Tatsuro

en Adachi, Tatsuro

Osanai, Yasuhito

× Osanai, Yasuhito

en Osanai, Yasuhito

Nakano, Nobuhiko

× Nakano, Nobuhiko

en Nakano, Nobuhiko

Toyoshima, Tsuyoshi

× Toyoshima, Tsuyoshi

en Toyoshima, Tsuyoshi

馬場, 壮太郎

× 馬場, 壮太郎

ja 馬場, 壮太郎

上里, 萌子

× 上里, 萌子

ja 上里, 萌子

外田, 智千

× 外田, 智千

ja 外田, 智千

足立, 達朗

× 足立, 達朗

ja 足立, 達朗

小山内, 康人

× 小山内, 康人

ja 小山内, 康人

中野, 伸彦

× 中野, 伸彦

ja 中野, 伸彦

豊島, 剛志

× 豊島, 剛志

ja 豊島, 剛志

アクセス権
アクセス権 open access
アクセス権URI http://purl.org/coar/access_right/c_abf2
主題
言語 ja
主題Scheme Other
主題 Sør Rondane Mountains
内容記述
内容記述タイプ Other
内容記述 Retrograde metamorphic P-T paths of garnet—pyroxene—bearing mafic gneisses from the Brattnipene nunataks in Sør Rondane Mountains, East Antarctica, were examined. The majority of samples preserve irregular—shaped garnet coexisting with clinopyroxene, quartz and plagioclase that developed around magnetite, ilmenite and orthopyroxene. The garnet contains fine—grained worm—like quartz inclusions. The occurrences are common in other mafic gneisses in northern Brattnipene and are interpreted as isobaric cooling textures. In another sample, garnet porphyroblasts have been replaced by symplectites of fine orthopyroxene and plagioclase. The mineral textures indicate near isothermal decompression. Retrograde P-T conditions estimated from rock containing orthopyroxene—plagioclase symplectite are within the range of 6.5 ~ 7.2 kbar, 700 ~ 780℃. Previous reports have revealed that metamorphism around Brattnipene is characterized by counterclockwise P-T path involving near—isobaric cooling. Our new finding suggests that metamorphic rocks formed by isothermal decompression should be present at higher altitude in the Brattnipene or relevant nunataks.
内容記述タイプ Other
内容記述 紀要論文
出版者
言語 ja
出版者 琉球大学教育学部
言語
言語 eng
資源タイプ
資源タイプ departmental bulletin paper
資源タイプ識別子 http://purl.org/coar/resource_type/c_6501
出版タイプ
出版タイプ VoR
出版タイプResource http://purl.org/coar/version/c_970fb48d4fbd8a85
識別子
識別子 http://hdl.handle.net/20.500.12000/39207
識別子タイプ HDL
収録物識別子
収録物識別子タイプ ISSN
収録物識別子 1345-3319
収録物識別子タイプ NCID
収録物識別子 AA11393705
収録物名
言語 ja
収録物名 琉球大学教育学部紀要=Bulletin of Faculty of Education University of the Ryukyus
書誌情報
号 92, p. 161-177
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