WEKO3
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Oxygen isotopic compositions of petrographically described inclusions from Antarctic unequilibrated ordinary chondrites
https://nipr.repo.nii.ac.jp/records/1568
https://nipr.repo.nii.ac.jp/records/1568190d1280-40c2-4146-8ddc-54a95ee4de89
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 | 1983-12-01 | |||||
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 | |||||
ページ属性 | ||||||
内容記述タイプ | Other | |||||
内容記述 | P(論文) | |||||
著者名(英) |
Onuma, Naoki
× Onuma, Naoki× Ikeda, Yukio× Mayeda, T.K.× Clayton, R.N.× Yanai, Keizo |
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著者所属(英) | ||||||
en | ||||||
Department of Earth Sciences, Faculty of Science,Ibaraki University/Department of Earth Sciences, Faculty of Science, Ibaraki University/Enrico Fermi Institute, The University of Chicago/Enrico Fermi Institute, The University of Chicago/National Institute of Polar Research | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | Several inclusions from the Antarctic unequilibrated ordinary chondrites (ALH-764 (LL3), ALH-77015 (L3) and Y-790448 (L3)) were excavated and their petrography, chemical and oxygen isotopic compositions were determined. The coherent data indicates that precursors of the ordinary chondrites consist of a mixture of two different solid materials. One is a pre-existing solid enriched in albite component and depleted in ^<16>O component and the other is a solid depleted in albite component and enriched in ^<16>O component. The latter solid material may be an evaporation residue of the former solid material in an ambient gas. | |||||
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 30, p. 306-314, 発行日 1983-12 |