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  1. 040 理学部
  2. 0402 紀要
  3. 04021 Journal of the Faculty of Science, Shinshu University
  4. Vol. 05

Uranocircite from Ogitsubo, Iida City, Nagano Prefecture

http://hdl.handle.net/10091/10443
http://hdl.handle.net/10091/10443
cf611182-f8cc-444d-8e25-381a3de0c7c7
名前 / ファイル ライセンス アクション
Science05-01-07.pdf Science05-01-07.pdf (1.8 MB)
Item type 紀要論文 / Departmental Bulletin Paper(1)
公開日 2010-10-06
タイトル
言語 en
タイトル Uranocircite from Ogitsubo, Iida City, Nagano Prefecture
言語
言語 eng
資源タイプ
資源 http://purl.org/coar/resource_type/c_6501
タイプ departmental bulletin paper
著者 WATANABE, KOJI

× WATANABE, KOJI

WEKO 37292

en WATANABE, KOJI

Search repository
出版者
出版者 信州大学理学部
引用
内容記述タイプ Other
内容記述 信州大学理学部紀要 5(1): 65-78(1970)
書誌情報 信州大学理学部紀要

巻 5, 号 1, p. 65-78, 発行日 1970-10-05
抄録
内容記述タイプ Abstract
内容記述 Uranocircite, a hydrated phase of barium and hexavalent uranium, Ba(UO₂)₂・(PO⁴)₂・8H₂O, was identified in the oxidation zone of Ogitsubo in the "Iida radioactiveanomlous area" in 1968. This yellow green mineral occurred in fine arkosic silt and white fissure clay (montmorillonite) which were deposited in the basal part of Miocene sediments just above the unconformity. Uranocircite, a sort of uranium mica minerals, is rarely found in ordinary uranium deposits, because barium in the mineral is easily replaced by such an element as calcium. Basement granite of this area contains abnormally rich thorium, while a relatively large amount of monazite, (La, Ce, Th, Y)・PO₄, is found in several localities of this district. Around the crystals of monazite included in biotite intense pleochroic haloes are observed under the microscope. Perhaps these environmental conditions led the generation of the barium-bearing uranophosphate mineral as secondary ore.
資源タイプ(コンテンツの種類)
内容記述タイプ Other
内容記述 Article
ISSN
収録物識別子タイプ PISSN
収録物識別子 0583-063X
書誌レコードID
収録物識別子タイプ NCID
収録物識別子 AA00697923
出版タイプ
出版タイプ VoR
出版タイプResource http://purl.org/coar/version/c_970fb48d4fbd8a85
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