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PETROGENESIS OF THE META-TRONDHJEMITES FROM CAPE HINODE, EAST ANTARCTICA
https://doi.org/10.15094/00002847
https://doi.org/10.15094/000028474f68693f-51ce-4c6d-bde8-4690b4dfacbc
名前 / ファイル | ライセンス | アクション |
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KJ00002368120 (1.1 MB)
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Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
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公開日 | 1997-09-01 | |||||
タイトル | ||||||
タイトル | PETROGENESIS OF THE META-TRONDHJEMITES FROM CAPE HINODE, EAST ANTARCTICA | |||||
言語 | ||||||
言語 | eng | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | eclogite | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | Lutzow-Holm Complex | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | MORB | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | slab | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | trondhjemite | |||||
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 | 10.15094/00002847 | |||||
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) | |||||
論文名よみ | ||||||
その他のタイトル | PETROGENESIS OF THE META-TRONDHJEMITES FROM CAPE HINODE, EAST ANTARCTICA | |||||
著者名よみ |
イケダ, ヤスオ
× イケダ, ヤスオ× シライシ, カズユキ× ヤナイ, ケイゾウ |
|||||
著者名(英) |
IKEDA, Yasuo
× IKEDA, Yasuo× SHIRAISHI, Kazuyuki× YANAI, Keizo |
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著者所属(英) | ||||||
en | ||||||
Hokkaido University of Education at Kushiro | ||||||
著者所属(英) | ||||||
en | ||||||
National Institute of Polar Research | ||||||
著者所属(英) | ||||||
en | ||||||
Faculty of Technology, Iwate University | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | Meta-trondhjemites (ca. 1000 Ma) from Cape Hinode, Lutzow-Holm Complex (LHC), East Antarctica are characterized by relatively high Al (Al_2O_3>15% at 70% SiO_2) and Sr, and low Y and Yb contents, which are chemically similar to Archaean trondhjemites and adakites. Trace element modelings of the partial melting of MORB suggest that igneous protoliths of the meta-trondhjemites were derived by partial melting of a basaltic source material under garnet stability P-T conditions. We suggest that a young hot subducting plate along LHC at 1000 Ma may have reached elevated temperatures which initiated melting of the slab. | |||||
雑誌書誌ID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AA1072335X | |||||
書誌情報 |
Proceedings of the NIPR Symposium on Antarctic Geosciences 巻 10, p. 102-110, 発行日 1997-09 |
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出版者 | ||||||
出版者 | National Institute of Polar Research |