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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.16 (Mar. 2003)

Primitive clasts in the Dar al Gani 319 polymict ureilite: Precursors of the ureilites

https://doi.org/10.15094/00006029
https://doi.org/10.15094/00006029
b98752cd-2012-44cb-8459-f0b9376c8ef6
名前 / ファイル ライセンス アクション
KJ00000040865.pdf KJ00000040865 (2.1 MB)
license.icon
Item type 紀要論文(ELS) / Departmental Bulletin Paper(1)
公開日 2003-03-01
タイトル
言語
言語 eng
キーワード
主題Scheme Other
主題 ureilites, DaG 319 polymict ureilite, primitive clasts, oxygen isotopes of clasts, ureilite precursors
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 10.15094/00006029
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) Ikeda,Yukio

× Ikeda,Yukio

WEKO 9926

en Ikeda,Yukio

Search repository
Kita,Noriko T.

× Kita,Noriko T.

WEKO 43674

en Kita,Noriko T.

Search repository
Morishita,Yuichi

× Morishita,Yuichi

WEKO 43675

en Morishita,Yuichi

Search repository
Weisberg,Michael K.

× Weisberg,Michael K.

WEKO 43676

en Weisberg,Michael K.

Search repository
著者所属(英)
en
Faculty of Science, Ibaraki University/Geological Survey of Japan, AIST/Geological Survey of Japan, AIST/Department of Physical Science,Kingsborough College (CUNY)
抄録(英)
内容記述タイプ Other
内容記述 Primitive clasts in the polymict ureilite Dar al Gani (DaG) 319 include dark clasts, sulfide- or metal-rich clasts, and unusual chondritic fragments. The dark clasts consist mainly of phyllosilicates, sulfides and magnetite with or without fayalitic olivine. The sulfide-rich clasts consist of a silicate-rich matrix and heterogeneously distributed sulfide. The metal-rich clasts consist of a silicate-rich matrix with variable amounts of metal. The unusual chondritic fragments are chondrule and equilibrated chondrite fragments. Oxygen isotopic compositions of the silicate-rich matrices in the sulfide-rich or metal-rich clasts plot on the carbonaceous chondrite anhydrous mineral (CCAM) mixing line between Allende matrix and a dark clast in the Nilpena polymict ureilite. Their oxygen isotopic compositions are similar to those of the monomict ureilites. Considering its chondritic composition and oxygen isotopic composition, the silicate-rich matrix of the sulfide-rich clasts is the best candidate for the ureilite precursors. However, the matrix has an Mg/(Mg+Fe) ratio (mg ratio) of 0.56 and is too ferroan to produce the monomict ureilites with mg ratios of 0.74-0.95. Therefore, it may have experienced various degrees of reduction to produce precursors with the mg ratios, needed to form the monomict ureilites as residues during fractional melting. Oxygen isotopic compositions of the unusual chondritic fragments plot near the ordinary chondrites on a 3-isotope diagram, suggesting that they have no direct genetic relationship to the monomict ureilites. They were projectiles that collided with the ureilite parent body (UPB).
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 16, p. 105-127, 発行日 2003-03
出版者
出版者 National Institute of Polar Research
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