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Redistribution of REE, Pb and U by supergene weathering studied from in-situ isotopic analyses of the Bangombe' natural reactor, Gabon

https://hiroshima.repo.nii.ac.jp/records/2006931
https://hiroshima.repo.nii.ac.jp/records/2006931
d8c1b18d-40b1-4bc3-8c46-8c972909fc97
名前 / ファイル ライセンス アクション
GCA_71_4716.pdf GCA_71_4716.pdf (2.5 MB)
Item type デフォルトアイテムタイプ_(フル)(1)
公開日 2023-03-18
タイトル
タイトル Redistribution of REE, Pb and U by supergene weathering studied from in-situ isotopic analyses of the Bangombe' natural reactor, Gabon
言語 en
作成者 Kikuchi, M.

× Kikuchi, M.

en Kikuchi, M.

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Hidaka, Hiroshi

× Hidaka, Hiroshi

en Hidaka, Hiroshi

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Horie, K.

× Horie, K.

en Horie, K.

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Gauthier-Lafaye, F.

× Gauthier-Lafaye, F.

en Gauthier-Lafaye, F.

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アクセス権
アクセス権 open access
アクセス権URI http://purl.org/coar/access_right/c_abf2
権利情報
権利情報 Copyright(c) 2007 Pergamon-Elsevier Science Ltd
主題
主題Scheme NDC
主題 450
内容記述
内容記述 The isotopic analyses of rare earth elements (REE), Pb and U in several kinds of minerals from the clay and black shale layers above the Bangombe natural reactor, Gabon, were performed using a sensitive high-resolution microprobe (SHRIMP) to investigate the migration and retardation processes of fission products released from the reactor. REE isotopic data of the secondary minerals found in clays and black shales show that most of fission products were effectively trapped in the clays and not distributed into the black shales over the clays, which reveals that the clays play an important role in preventing fission products from spreading. Zircon crystals in the clays heterogeneously contain high-U regions (up to 28.3 wt%) with normal U-235/U-238 ratios (=0.00725) and significant amounts of fissiogenic REE, which suggest the occurrence of significant chemical fractionation between REE and U during the dissolution of reactor uraninite and the recrystallization of secondary U minerals. The Pb data suggest that galena grains in the clays were also formed by the mixing of the two components during a recent alteration event, and that a significant amount of Pb was derived from 2.05-Ga-old original uraninite rather than reactor uraninite. The U-Pb systematics of zircon provide chronological information on the old igneous activity associated with the basement rock formation at 2.8 Ga and geochemical evidence of the incomplete mixing of independent Pb and U sources. This result is consistent with previous chronological results in this area.
言語 en
出版者
出版者 Pergamon-Elsevier Science Ltd
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 journal article
出版タイプ
出版タイプ AO
出版タイプResource http://purl.org/coar/version/c_b1a7d7d4d402bcce
関連情報
識別子タイプ DOI
関連識別子 10.1016/j.gca.2007.07.016
関連情報
関連タイプ isVersionOf
識別子タイプ DOI
関連識別子 http://dx.doi.org/10.1016/j.gca.2007.07.016
収録物識別子
収録物識別子タイプ ISSN
収録物識別子 0016-7037
収録物識別子
収録物識別子タイプ NCID
収録物識別子 AA00655038
開始ページ
開始ページ 4716
書誌情報 Geochimica et Cosmochimica Acta
Geochimica et Cosmochimica Acta

巻 71, 号 19, p. 4716-4726, 発行日 2007-10
旧ID 21460
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