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  1. 紀要類
  2. Memoirs of National Institute of Polar Research. Special issue (ISSN 0386-0744)
  3. No.20 (Dec. 1981)

Did diogenites form from diogenites?: A case of Yamato diogenites

https://nipr.repo.nii.ac.jp/records/1206
https://nipr.repo.nii.ac.jp/records/1206
8c554ba6-1dc5-4aa4-81b3-081a8abef22d
名前 / ファイル ライセンス アクション
KJ00000011732.pdf KJ00000011732 (778.8 kB)
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Item type 紀要論文(ELS) / Departmental Bulletin Paper(1)
公開日 1981-12-01
タイトル
タイトル Did diogenites form from diogenites?: A case of Yamato diogenites
言語 en
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) Masuda, Akimasa

× Masuda, Akimasa

en Masuda, Akimasa

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Nakamura, Noboru

× Nakamura, Noboru

en Nakamura, Noboru

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Shimizu, Hiroshi

× Shimizu, Hiroshi

en Shimizu, Hiroshi

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Tanaka, Tsuyoshi

× Tanaka, Tsuyoshi

en Tanaka, Tsuyoshi

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著者所属(英)
言語 en
値 Department of Earth Sciences, Faculty of Science, Kobe University/Department of Earth Sciences, Faculty of Science, Kobe University/Department of Earth Sciences, Faculty of Science, Kobe University/Geological Survey of Japan
抄録(英)
内容記述タイプ Other
内容記述 It has been found that the REE distribution in Y-74010 is considerably different between two adjacent fragments, sizes of which are at least 500mg, a fact indicative of patchy heterogeneity. In addition, it is worthwhile to note that the abundance ratios between two fragments in question are a linear function of atomic number. On the other hand, Y-74013 can be interpreted as a mixture of two distinct constituents, i.e., relatively coarse-grained pyroxene and much finer pyroxenic remnant component. It is noted that these two constituents of Y-74013 can correspond to two different kinds of parts represented by macroscopically separated patches of Y-74010 mentioned above. These observations coupled with the basically linear abundance ratios relative to atomic number suggest that (1) intense melting took place for a parental body of the Yamato diogenites, (2) two separate components reflect the coexisting solid and liquid phases and (3) the solid phase was formed from liquid, transiently as a low-Ca clinopyroxene, which subsequently changed into orthopyroxene as a finally stable form. Also it is an interesting fact that the apparent REE partition function pertaining to Y-692 appears to show discrete (quantum-like) effect.
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. 100-105, 発行日 1981-12
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