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Noble gases in Yamato-791197: Evidence for lunar highland origin
https://nipr.repo.nii.ac.jp/records/1958
https://nipr.repo.nii.ac.jp/records/1958ccbaac2d-cd4e-4913-a305-d8c39b183843
名前 / ファイル | ライセンス | アクション |
---|---|---|
KJ00000012512.pdf (1.2 MB)
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Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
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公開日 | 1986-07-01 | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | Noble gases in Yamato-791197: Evidence for lunar highland origin | |||||
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) |
Takaoka, Nobuo
× Takaoka, Nobuo |
|||||
著者所属(英) | ||||||
en | ||||||
Department of Earth Sciences, Faculty of Science, Yamagata University | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | Concentrations and isotopic compositions of five stable noble gases were determined for a whole rock sample and a white clast prepared from the Yamato-791197 breccia. The whole rock contains large amounts of trapped gases originating from solar wind implantation. Relative elemental abundances and isotopic compositions of trapped gases indicate the possible origin of the Y-791197 meteorite from lunar highland regolith. The high concentrations of both trapped and spallogenic gases in the whole rock and the cosmogenic ^<131>Xe/^<126>Xe ratio in the white clast suggest that the meteorite resided at a low average cosmic-ray shielding less than 65g/(cm)^2. An exposure age of 910±60 Ma is tentatively estimated for the whole rock, whereas the exposure age for the white clast is shorter by a factor of about three. | |||||
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 41, p. 124-132, 発行日 1986-07 |