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Petrological note on some metamorphic rocks from Skallen, East Antarctica (abstract)
https://nipr.repo.nii.ac.jp/records/1480
https://nipr.repo.nii.ac.jp/records/1480223c6a35-897b-41ab-84ee-a791afa1fcac
名前 / ファイル | ライセンス | アクション |
---|---|---|
KJ00000012113 (81.9 kB)
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Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
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公開日 | 1983-10-01 | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | Petrological note on some metamorphic rocks from Skallen, East Antarctica (abstract) | |||||
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) |
Suzuki, Morihisa
× Suzuki, Morihisa× Yoshida, Masaru |
|||||
著者所属(英) | ||||||
en | ||||||
Institute of Geology and Mineralogy, Faculty of Science, Hiroshima University | ||||||
著者所属(英) | ||||||
en | ||||||
Department of Geosciences, Faculty of Science, Osaka City University | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | A preliminary petrography of a paragneiss and two metabasites from the Skallen area of the Lutzow-Holm Bay region is given. The paragneiss has the stable association of garnet ((Gr)_<2.2-3.3>(Alm)_<60.9-62.2>(Pyr)_<34.0-36.2>(Spes)_<0.7-0.8>)+sillimanite+K feldspar+plagioclase (X_<ca>=0.23)+quartz±biotite+rutile+ilmenite, and metabasites, orthopyroxene (X_<Fe>=0.56 to 0.59)+clinopyroxene (X_<Fe>=0.44 to 0.45)+garnet ((Gr)_<18.8-26.7>(Alm)_<56.6-63.4>(Pyr)_<11.7-14.3>(Spes)_<2.9-4.4>)+plagioclase (X_<ca>=0.65 to 0.87)+quartz±hornblende+ilmenite and magnetite. Based on the calculations following some geothermometers (garnet-biotite, THOMPSON : Am. J. Sci., 276,425,1976 and orthopyroxene-clinopyroxene, WOOD and BANNO : Contrib. Mineral. Petrol., 42,109,1973,subtracting 50℃) and geobarometers (garnet-sillimanite-plagioclase, GHENT : Am. Mineral., 61,710,1976 and garnet-orthopyroxene-plagioclase, WELLS : J. Petrol., 20,187,1979), the metamorphic conditions have been inferred to be graded up to 725±25℃ and 6.3±1.3kb. These temperature and pressure values are considered to represent the conditions of some stage during the dominant granulite facies metamorphism in the area, although microstructures of rocks may suggest that some superposed metamorphic events took place in the area. Further detailed explanations, especially on microstructures of rocks and their correlation with the mineral chemistry, are left for future studies. | |||||
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 28, p. 217, 発行日 1983-10 |