WEKO3
アイテム
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Classification of several Yamato-75 chondrites (III)
https://nipr.repo.nii.ac.jp/records/1203
https://nipr.repo.nii.ac.jp/records/1203c3b9cabf-ad4c-4b78-9962-85c3097314e2
名前 / ファイル | ライセンス | アクション |
---|---|---|
KJ00000011729 (2.1 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 | Classification of several Yamato-75 chondrites (III) | |||||
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 | All the chondrites from the Yamato-75108 to -75257 have been considered to be originally one single body of meteorite which was broken into many fragments during its passage through the atmosphere. An electron microprobe analyzer was used to determine the chemical compositions of olivines and orthopyroxenes in five chondrites, i.e. Yamato-75135,93,-75136,93,-75140,50,-75140,51 and -75146,91. These chondrites are classified on the basis of textural characteristics of chondrule, matrix, igneous glass and secondary feldspar, and on the compositions of olivines and orthopyroxenes. The experimental results show that the chondrites are tentatively assigned to L group and petrologic type 4-5. These chondrites were possibly one single meteorite originally, together with eleven chondrites reported by MATSUMOTO et al. (Mem. Natl Inst. Polar Res., Spec. Issue, 12,72,1979), and MATSUMOTO and HAYASHI (Ibid, 17,21,1980). An unclassified chondrite, Yamato-75271,91,which was found at 5km south of the area where the chondrites Yamato-75108 to -75257 were collected, is determined to be of L group and petrologic type 4-5 based on the same analytical method as the above five chondrites. The chemical compositions of plagioclases in these six chondrites show a wide variation from oligoclase to andesine. | |||||
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. 53-68, 発行日 1981-12 |