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PRELIMINARY RESULT FOR THE Sm-Nd WHOLE-ROCK AGE OF THE METAMORPHIC ROCKS FROM MOUNT PARDOE IN THE NAPIER COMPLEX, EAST ANTARCTICA
https://doi.org/10.15094/00002756
https://doi.org/10.15094/0000275648dd0ca3-99d6-4637-b25e-495537f8985e
名前 / ファイル | ライセンス | アクション |
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Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
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公開日 | 1994-09-01 | |||||
タイトル | ||||||
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 | 10.15094/00002756 | |||||
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 | PRELIMINARY RESULT FOR THE Sm-Nd WHOLE-ROCK AGE OF THE METAMORPHIC ROCKS FROM MOUNT PARDOE IN THE NAPIER COMPLEX, EAST ANTARCTICA | |||||
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× カガミ, ヒロオ× タカハシ, ユウヘイ× イイズミ, シゲル× 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× KAGAMI, Hiroo× TAKAHASHI, Yuhei× IIZUMI, Shigeru× OSANAI, Yasuhito× TSUCHIYA, Noriyoshi |
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著者所属(英) | ||||||
en | ||||||
Department of Natural Environment, Faculty of Human Development, Kobe University | ||||||
著者所属(英) | ||||||
en | ||||||
Institute for Study of the Earth's Interior, Okayama University | ||||||
著者所属(英) | ||||||
en | ||||||
Geological Survey of Japan | ||||||
著者所属(英) | ||||||
en | ||||||
Department of Geology, Faculty of Science, Shimane 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 Sm-Nd whole rock isochron age was determined for metamorphic rocks from Mount Pardoe, Napier Complex. Acidic gneiss (orthopyroxene-mesoperthite-quartz gneiss), being one of the main representative metamorphic rocks, gave an age of 2516±274 Ma with an initial ^<143>Nd/^<144>Nd ratio of 0.50914±0.00021. εNd values normalized to 2516 Ma for individual acidic gneiss range from -3.7 to -7.0. This Sm-Nd whole-rock isochron age indicates a major period of equilibration of the isotopic system on a whole-rock scale at 2516±274 Ma. | |||||
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 7, p. 115-121, 発行日 1994-09 |
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出版者 | ||||||
出版者 | National Institute of Polar Research |