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Resetting and closing codition of Rb-Sr whole-rock isochron system: some samples of metamorphic and granitic rocks from the Gondwana super-continent and Japan Arc
https://doi.org/10.15094/00003130
https://doi.org/10.15094/000031300fe1bd08-3a08-434c-bcdc-2f28010d6b4e
名前 / ファイル | ライセンス | アクション |
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KJ00000044124 (2.1 MB)
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Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
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公開日 | 2003-10-01 | |||||
タイトル | ||||||
タイトル | Resetting and closing codition of Rb-Sr whole-rock isochron system: some samples of metamorphic and granitic rocks from the Gondwana super-continent and Japan Arc | |||||
言語 | ||||||
言語 | eng | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | Rb-Sr whole-rock isochron age | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | metamorphism | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | Sr isotopic homogenization | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | partial melting | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | fluids | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | closure temperature | |||||
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 | 10.15094/00003130 | |||||
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(英) |
Kagami, Hiroo
× Kagami, Hiroo× Simura, Toshiaki× Yuhara, Masaki× Owada, Masaaki× Osanai, Yasuhito× Shiraishi, Kazuyuki |
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著者所属(英) | ||||||
en | ||||||
Graduate School of Science and Technology, Niigata University/Department of Geology, Niigata University/Department of Earth System Science, Fukuoka University/Department of Earth Sciences, Yamaguchi University/Department of Earth Sciences, Okayama University/National Institute of Polar Research | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | The closure temperature of the Rb-Sr whole-rock system for felsic rocks has been generally considered to be ca. 700゜C, but it falls to ca. 400゜C, as a result of efficient action of fluids,especially H_2O. Thus,the Rb-Sr whole-rock ages obtained by rocks collected from a single outcropto specimen-size are not always coincident with those of emplacement of granitic magma or partial melting under high grade metamorphism.Although the Rb-Sr whole-rock isochron ages of metamorphic rocks collected from a wide area have been sometimes interpreted as those of metamorphism,careful consideration for these ages is needed. | |||||
雑誌書誌ID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AA1130866X | |||||
書誌情報 |
Polar geoscience 巻 16, p. 227-242, 発行日 2003-10 |
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出版者 | ||||||
出版者 | National Institute of Polar Research |