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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.17 (Sep. 2004)

Variable initial zoning profiles and Fe-Mg diffusion coefficients for olivine: Effects on cooling rates calculated by diffusion modeling in a pallasite

https://doi.org/10.15094/00006054
https://doi.org/10.15094/00006054
42b17ef7-a0cd-4a29-91a1-3180e4b51b66
名前 / ファイル ライセンス アクション
KJ00002352202.pdf KJ00002352202 (525.7 kB)
license.icon
Item type 紀要論文(ELS) / Departmental Bulletin Paper(1)
公開日 2004-09-01
タイトル
言語
言語 eng
キーワード
言語 en
主題Scheme Other
主題 diffusion, pallasite, olivine, cooling rate, chemical zoning
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 10.15094/00006054
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)
論文名よみ
その他のタイトル Variable initial zoning profiles and Fe-Mg diffusion coefficients for olivine: Effects on cooling rates calculated by diffusion modeling in a pallasite
著者名(英) Miyamoto,Masamichi

× Miyamoto,Masamichi

WEKO 9949

en Miyamoto,Masamichi

Search repository
Monkawa,Akira

× Monkawa,Akira

WEKO 43725

en Monkawa,Akira

Search repository
Koizumi,Eisuke

× Koizumi,Eisuke

WEKO 43726

en Koizumi,Eisuke

Search repository
Mikouchi,Takashi

× Mikouchi,Takashi

WEKO 43727

en Mikouchi,Takashi

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著者所属(英)
en
Space and Planetary Science, Graduate School of Science,University of Tokyo/Space and Planetary Science, Graduate School of Science,University of Tokyo/Space and Planetary Science, Graduate School of Science,University of Tokyo/Space and Planetary Science, Graduate School of Science,University of Tokyo
抄録(英)
内容記述タイプ Other
内容記述 Because chemical zoning of minerals contains information about the thermal history of the parent body, the cooling rate or burial depth can be calculated by solving the diffusion equation. Several factors influence the results of these calculations. We evaluated the cooling rate (and burial depth) calculated by using different initial (starting) zoning profiles and different diffusion coefficients on the basis of the Fe-Mg chemical zoning profile observed for pallasite (Esquel) olivine. Uncertainties in initial compositional profile and Fe-Mg diffusion coefficient in olivine both lead to error in model cooling rates. Discrepancies between different experimentally determined diffusion coefficients lead to uncertainties in model cooling rate that exceed those due to initial zoning profiles by one order of magnitude. These results highlight the need for accurate determination of diffusion coefficients in olivine.
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 17, p. 252-258, 発行日 2004-09
出版者
出版者 National Institute of Polar Research
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