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On homogeneity of the Yamato-75110 chondrite
https://nipr.repo.nii.ac.jp/records/1207
https://nipr.repo.nii.ac.jp/records/1207530bc86d-3ab7-4ae3-9100-4f78c28d97bc
名前 / ファイル | ライセンス | アクション |
---|---|---|
KJ00000011733 (1.5 MB)
|
Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
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公開日 | 1981-12-01 | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | On homogeneity of the Yamato-75110 chondrite | |||||
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) |
Matsumoto, Yukio
× Matsumoto, Yukio× Hayashi, Masao× Daishi, Masahiro× Miura, Yasunori |
|||||
著者所属(英) | ||||||
en | ||||||
Department of Mineralogical Sciences and Geology, Faculty of Science, Yamaguchi University/Research Institute of Industrial Science, Kyusyu University/Department of Marine Sciences, Faculty of Science, University of the Ryukyus/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 | The Yamato-75108 to -75257 chondrites are considered to be originally one meteorite which was broken into many fragments (MATSUMOTO : Mem. Natl Inst. Polar Res., Spec. Issue, 8,38,1978; MATSUMOTO et al. : Ibid., 12,72,1979; MATSUMOTO and HAYASHI : Ibid., 17,21,1980). Electron microprobe analyses have been made on olivine and orthopyroxene, and microscopic studies on four different portions (such as Nos. 90,91,93 and 95) of the Yamato-75110 chondrite. Textural characters of chondrules, matrix, igneous glass and secondary feldspar, and the mean composition, mean deviation, and percent mean deviation of the iron contents of olivines and orthopyroxenes are given. The value of % M.D. for the olivine in the Yamato-75110 chondrite ranges from 2.02 to 2.98; but that in the matrix is from 1.79 to 2.12,and that in chondrule is from 0.88 to 2.05. The value of % M.D. for the orthopyroxene in this chondrite ranges from 2.38 to 5.27; but that in the matrix is from 2.15 to 7.17,and that in the chondrule is from 2.12 to 4.43. Such a chemical variety of the Yamato-75110 chondrite is observed cleary in this study. However, this chondrite is classified as L group and petrologic type 4-5. | |||||
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 20, p. 106-118, 発行日 1981-12 |