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Hornblende gneisses from Syowa Station, East Antarctica
https://nipr.repo.nii.ac.jp/records/1785
https://nipr.repo.nii.ac.jp/records/17857d9b8b48-12e7-44c2-9468-bfb8b1cd51cd
名前 / ファイル | ライセンス | アクション |
---|---|---|
KJ00000012417 (2.9 MB)
|
Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
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公開日 | 1985-09-01 | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | Hornblende gneisses from Syowa Station, East Antarctica | |||||
言語 | ||||||
言語 | eng | |||||
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 | |||||
ページ属性 | ||||||
内容記述タイプ | Other | |||||
内容記述 | P(論文) | |||||
著者名(英) |
Hiroi, Yoshikuni
× Hiroi, Yoshikuni× Onuki, Hitoshi |
|||||
著者所属(英) | ||||||
en | ||||||
Department of Earth Sciences, Faculty of Science, Chiba University | ||||||
著者所属(英) | ||||||
en | ||||||
Department of Earth Sciences, Faculty of Science, Hirosaki University | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | Pyroxene gneiss (charnockitic gneiss), local hornblende gneiss (bleached part of pyroxene gneiss), biotite schist, and pegmatite were newly analyzed chemically. The results together with the published analyses of regional hornblende gneisses and pyroxene gneisses show that regional hornblende gneisses generally have higher rock oxidation ratios and MgO/(MgO+FeO) ratios than pyroxene gneisses and local hornblende gneiss, in harmony with the differences in oxide mineral assemblages and in microprobe analyses of minerals. Such differences correspond to the factors controlling the stabilities of amphiboles, and suggest that regional hornblende gneisses are the products of low granulite-facies metamorphism. The difference in mineralogy among pyroxene gneiss, local hornblende gneiss, and biotite schist may be shown by an isochemical reaction. | |||||
雑誌書誌ID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AA00733561 | |||||
書誌情報 |
Memoirs of National Institute of Polar Research. Special issue 巻 37, p. 63-81, 発行日 1985-09 |