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An inclusion of ALH-77004: A possible surface regolith of L chondrite parent body
https://nipr.repo.nii.ac.jp/records/1550
https://nipr.repo.nii.ac.jp/records/1550a5ce80ed-a15a-4f33-b8db-013e74192443
名前 / ファイル | ライセンス | アクション |
---|---|---|
KJ00000012183.pdf (1.3 MB)
|
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 | en | |||||
タイトル | An inclusion of ALH-77004: A possible surface regolith of L chondrite parent body | |||||
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) |
Matsunami, Satoshi
× Matsunami, Satoshi |
|||||
著者所属(英) | ||||||
en | ||||||
Geological Institute, Faculty of Science, University of Tokyo | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | An inclusion in ALH-77004 (H4 chondrite) consists of four different constituents with varying degree of recrystallization; (1) moderately to highly recrystallized lithic and chondrule fragments (fayalite-rich group), (2) unequilibrated chondrules (fayalite-poor group), (3) fine-grained dark clastic matrix, and (4) particles of Fe-Ni metal, troilite, and chromite. From petrological examinations of these constituents, it is suggested that the inclusion was a surface regolith of the L chondrite parent body formed by repetitive impact cratering processes extended to various depths of the body. | |||||
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. 36-44, 発行日 1983-12 |