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PRELIMINARY PETROLOGICAL STUDIES OF THE GRANITIC ROCKS IN THE SØR RONDANE MOUNTAINS, EAST ANTARCTICA
https://doi.org/10.15094/00002721
https://doi.org/10.15094/00002721cb755414-c151-4f37-8bcd-30a9393482bd
名前 / ファイル | ライセンス | アクション |
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KJ00002368351 (2.5 MB)
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Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
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公開日 | 1993-09-01 | |||||
タイトル | ||||||
タイトル | PRELIMINARY PETROLOGICAL STUDIES OF THE GRANITIC ROCKS IN THE SØR RONDANE MOUNTAINS, 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 | |||||
ID登録 | ||||||
ID登録 | 10.15094/00002721 | |||||
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) | |||||
著者名よみ |
タイノショウ, ヨシアキ
× タイノショウ, ヨシアキ× タカハシ, ユウヘイ× マエカワ, ヒロカズ× オサナイ, ヤスヒト× ツチヤ, ノリヨシ |
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著者名(英) |
TAINOSHO, Yoshiaki
× TAINOSHO, Yoshiaki× TAKAHASHI, Yuhei× MAEKAWA, Hirokazu× OSANAI, Yasuhito× TSUCHIYA, Noriyoshi |
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著者所属(英) | ||||||
en | ||||||
Division of Natural Environment, Faculty of Human Development, Kobe University | ||||||
著者所属(英) | ||||||
en | ||||||
Geological Survey of Japan | ||||||
著者所属(英) | ||||||
en | ||||||
Department of Earth and Planetary Sciences, Faculty of Science, Kobe University | ||||||
著者所属(英) | ||||||
en | ||||||
Department of Earth Sciences and Astronomy, Fukuoka University of Education | ||||||
著者所属(英) | ||||||
en | ||||||
Department of Resources Engineering, Faculty of Engineering, Tohoku University | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | The Sør Rondane Mountains mainly consist of Proterozoic metamorphic rocks and various kinds of Late Proterozoic to Early Paleozoic granitic rocks. The Early Paleozoic granitic rocks can be divided into two types, concordant granites and discordant granites. Chemical analyses of major and trace elements for the Early Paleozoic granitic rocks are presented. The discordant granites are characterized by high Ba, Sr and alkalies. In contrast, the concordant granites are high in Y and Nb and slightly low in CaO, Cr and Sr compared with the discordant granites. Most of the concordant granites are classified as within plate granites and the discordant granites as volcanic arc granites, based on trace elements. Mineral compositions in the granitic rocks are also related to the two granite types. Mg/(Mg+Fe) ratios of ferromagnesian minerals of the concordant granites are very low, while those of the discordant granites have intermediate Mg/(Mg+Fe) ratios. Anorthite contents of plagioclases in the concordant granites are low, while those of the discordant granites have slightly high anorthite content compared with those of the concordant granites. These chemical features and the Sr initial ratios may suggest that these two granite types were formed under different conditions. | |||||
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 6, p. 83-102, 発行日 1993-09 |
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出版者 | ||||||
出版者 | National Institute of Polar Research |