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  1. 極地研刊行誌
  2. 英文誌
  3. 南極隕石
  4. Antarctic meteorite research (ISSN 1343-4284)
  5. No.10 (Sep. 1997)

Chemical zoning of olivines in the Yamato-791717 CO3 chondrite

https://doi.org/10.15094/00005897
https://doi.org/10.15094/00005897
2fadb3c9-7d6f-4d9c-b665-b4a2bc417cc0
名前 / ファイル ライセンス アクション
KJ00000040889.pdf KJ00000040889 (1.6 MB)
license.icon
Item type 紀要論文(ELS) / Departmental Bulletin Paper(1)
公開日 1997-09-01
タイトル
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
ID登録
ID登録 10.15094/00005897
ID登録タイプ JaLC
ページ属性
内容記述タイプ Other
内容記述 P(論文)
著者名(英) Kaiden,Hiroshi

× Kaiden,Hiroshi

WEKO 9833

en Kaiden,Hiroshi

Search repository
Mikouchi,Takashi

× Mikouchi,Takashi

WEKO 43873

en Mikouchi,Takashi

Search repository
Nomura,Koji

× Nomura,Koji

WEKO 43874

en Nomura,Koji

Search repository
Miyamoto,Masamichi

× Miyamoto,Masamichi

WEKO 43875

en Miyamoto,Masamichi

Search repository
著者所属(英)
en
Mineralogical Institute, Graduate School of Science, University of Tokyo/Mineralogical Institute, Graduate School of Science, University of Tokyo/Mineralogical Institute, Graduate School of Science, University of Tokyo/Mineralogical Institute, Graduate School of Science, University of Tokyo
抄録(英)
内容記述タイプ Other
内容記述 The chemical zoning profiles of olivines in the Yamato (Y)-791717 CO3 chondrite have been analyzed in order to explore its thermal history. Two alternative models were applied to distinguish igneous processes from metamorphic features; they are fractional crystallization and diffusive modification of primary composition. It was clarified that chemical zoning of olivines in Y-791717 has been formed by a diffusion process, suggesting that this meteorite has been thermally metamorphosed. Thermal metamorphism of Y-791717 we have shown is consistent with that proposed on the basis of thermoluminescence investigation. A diffusion model also allows us to examine its thermal history in a quantitative way. Using a diffusion model, we have most successfully reproduced measured zoning profiles in isolated and chondrule olivine grains from Y-791717 in the temperature range 800-300℃. The temperature range is broadly consistent with the previously proposed peak metamorphic temperatures for CO3 chondrites.
雑誌書誌ID
収録物識別子タイプ NCID
収録物識別子 AA11182426
書誌情報 Antarctic meteorite research

巻 10, p. 181-190, 発行日 1997-09
出版者
出版者 National Institute of Polar Research
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