WEKO3
アイテム
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Opaque Minerals in the Yamato-74191 Chondrules
https://nipr.repo.nii.ac.jp/records/1091
https://nipr.repo.nii.ac.jp/records/1091d015489d-fa26-46e3-830a-cb04d66f288e
名前 / ファイル | ライセンス | アクション |
---|---|---|
KJ00000011617 (1.3 MB)
|
Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
---|---|---|---|---|---|---|
公開日 | 1980-12-01 | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | Opaque Minerals in the Yamato-74191 Chondrules | |||||
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) |
Kimura, Makoto
× Kimura, Makoto× Yagi, Kenzo× Onuma, Kosuke |
|||||
著者所属(英) | ||||||
en | ||||||
Department of Geology and Mineralogy, Faculty of Science, HokkaidoUniversity | ||||||
著者所属(英) | ||||||
en | ||||||
Department of Geology and Mineralogy, Faculty of Science, HokkaidoUniversity | ||||||
著者所属(英) | ||||||
en | ||||||
Department of Geology and Mineralogy, Faculty of Science, Hokkaido University | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | Opaque minerals occur often as phenocrysts in porphyritic chondrules. Troilite is common in comparison with metallic iron in chondrules, and is often distributed separately from metallic iron in a chondrule. Since some opaque minerals are included in silicate minerals, opaque minerals had crystallized in a chondrule before the crystallization of silicate minerals. Rare chromites are always in contact with troilites. These chromites, including some other meteoritic chromites, have cation deficiency in the B site. This cation deficiency may be interpreted by a substitution of 3Fe^<2+>=2Cr^<8+>+Vacancy. Chromites and olivines in chondrule crystallized in disequilibrium to each other. | |||||
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 17, p. 95-103, 発行日 1980-12 |