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Classification of several Yamato-75 chondrites (IV)
https://nipr.repo.nii.ac.jp/records/1376
https://nipr.repo.nii.ac.jp/records/1376ca180b72-0d44-4ceb-9d0f-e90c66b5065d
名前 / ファイル | ライセンス | アクション |
---|---|---|
KJ00000012010 (2.7 MB)
|
Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
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公開日 | 1982-12-01 | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | Classification of several Yamato-75 chondrites (IV) | |||||
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) |
Miura, Yasunori
× Miura, Yasunori× Matsumoto, Yukio |
|||||
著者所属(英) | ||||||
en | ||||||
Department of Mineralogical Sciences and Geology, Faculty of Science, Yamaguchi University | ||||||
著者所属(英) | ||||||
en | ||||||
Department of Mineralogical Sciences and Geology, Faculty of Science, Yamaguchi University | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | An electron microprobe analyzer was used to determine the chemical compositions of olivines and orthopyroxenes in six chondrites, i.e. Yamato-75119,91,-75124,91,-75125,91,-75126,91,-75128,92 and -75133,93. These chondrites are classified on the basis of textural characteristics of chondrules, matrix, plagioclase and igneous glass, and on the compositions of olivines and orthopyroxenes. The statistical analyses of the experimental results show that the chondrites Yamato-75119,91,-75125,91,-75126,91 and -75128,92 are tentatively assigned to L4∿5 [i.e. L4 (67%), (67%), (83%) and (83%), respectively], and that the chondrites Yamato-75124,91 and -75133,93 are assigned to L5∿4 [i.e. L5 (67%)] and LL4∿5 [i.e. L4 (67%)], respectively. These chondrites, except the chondrites Yamato-75133,93,were possibly one single meteorite originally which was broken into many fragments during passage through the atmosphere, together with seventeen chondrites previously reported. The chondrite Yamato-75133,93 is possibly a different fragment from the above seventeen chondrites. Another sample of the chondrite Yamato-75102,74 tentatively classified as L6∿5 chondrite from different sampling area, is determined to be of L4∿5 [i.e. L4 (67%)] chondrite based on the same analytical method as the above six chondrites. The chemical compositions of plagioclases in these seven chondrites show some variation in oligoclase compositions. | |||||
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 25, p. 1-16, 発行日 1982-12 |