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Geology of eastern Muhlig -Hofmannfjella and Filchnerfjella in Dronning Maud Land, East Antarctica; A preliminary report of a Japan-Norway-Germany joint geological investigation
https://doi.org/10.15094/00003125
https://doi.org/10.15094/00003125549c6e22-234e-4b50-a8ae-b5ae19f1354d
名前 / ファイル | ライセンス | アクション |
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KJ00000044119 (5.4 MB)
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Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
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公開日 | 2003-10-01 | |||||
タイトル | ||||||
タイトル | Geology of eastern Muhlig -Hofmannfjella and Filchnerfjella in Dronning Maud Land, East Antarctica; A preliminary report of a Japan-Norway-Germany joint geological investigation | |||||
言語 | ||||||
言語 | eng | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | central Dronning Maud Land | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | geology of Filchnerfjella | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | two-stage meta-morphism | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | Pan-African magmatism | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | Gondwana break-up | |||||
資源タイプ | ||||||
資源タイプ識別子 | http://purl.org/coar/resource_type/c_6501 | |||||
資源タイプ | departmental bulletin paper | |||||
ID登録 | ||||||
ID登録 | 10.15094/00003125 | |||||
ID登録タイプ | JaLC | |||||
ページ属性 | ||||||
内容記述タイプ | Other | |||||
内容記述 | P(論文) | |||||
著者名(英) |
Owada, Masaaki
× Owada, Masaaki× Baba, Sotaro× Laufer, Andreas L.× Elvevold, Synnoeve× Shiraishi, Kazuyuki× Jacobs, Joachim |
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著者所属(英) | ||||||
en | ||||||
Department of Earth Sciences, Yamaguchi University/Department of Natural Environment, University of the Ryukyus/Geologisch-Palaontologisches Institut, Johann Wolfgang Goethe-Universitat/Norwegian Polar Institute/National Institute of Polar Research/Universitat Bremen | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | The geological history of Filchnerfjella and surrounding areas (2゜E to 8゜E) in central Dronning Maud Land,East Antarctica,is constructed from metamorphic and igneous petrology,and structural investigations.The geology of Filchner-fjella consists mainly of metamorphic rocks accompanied by intrusive rocks.Two stages of metamorphism can be recognized in this area.The earlier stage metamorphism is defined as a porphyroblast stage (garnet,hornblende,and sillimanite stable), and the later one is recognized as a symplectic stage (orthopyroxene and cordieritestable).Taking metamorphic textures and geothermobarometries into account,the rocks experienced an early high-P/medium-T followed by a low-P and high-T stage. Partial melting took place during the low-P/high-T stage,because probable melt of leucocratic gneiss contains cordierite.The field relationships and petrography of the syenite at Filchnerfjella are similar to those of post-tectonic plutons from central Dronning Maud Land,and most of the post-tectonic intrusive rocks have within-plate geochemical features.The structural history in Filchnerfjella and surrounding areas can be divided into the Pan-African stage and the Meso to Cenozoic stage that relates to the break-up of Gondwana. | |||||
雑誌書誌ID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AA1130866X | |||||
書誌情報 |
Polar geoscience 巻 16, p. 108-136, 発行日 2003-10 |
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出版者 | ||||||
出版者 | National Institute of Polar Research |