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DOI10.1016/j.oregeorev.2021.104641
Occurrence and mechanism of uranium enrichment with a unique eolian sedimental environment in the Pengyang uranium deposit, Ordos Basin
Zhao, Hualei; Ao, Cong; Li, Jianguo; Chen, Lulu; Zhang, Bo; Miao, Peisen; Si, Qinghong; Zhu, Qiang; Yu, Rengan; Chen, Yin
通讯作者Zhao, HL ; Ao, C (corresponding author),China Geol Survey, Tianjin Ctr, Tianjin 300170, Peoples R China.
来源期刊ORE GEOLOGY REVIEWS
ISSN0169-1368
EISSN1872-7360
出版年2022
卷号141
英文摘要The Pengyang uranium deposit is a recently discovered large-scale uranium deposit in the Lower Cretaceous Luohe Formation in the southwestern Ordos Basin, China, and this high content of active uranium in the ore suggests that the Pengyang uranium deposit is generally suitable for in situ leaching mining. In this study, the uraniferous sandstones from the Luohe Formation were analyzed in detail. The mineral symbiosis and uranium occurrence state were studied using scanning electron microscopy, energy spectral analysis, backscattering detection, electron probe microanalysis, and sequential extraction procedures for uranium. Results show that the uranium minerals are mostly disseminated, clustered, or veinlet, being distributed along the edges and in the pores between detrital grains, and they are usually closely symbiotic with anatase, pyrite, apatite, and clay minerals. The uranium minerals are mainly pitchblende, with a small amount of coffinite. The results of sequential extraction procedures reveal that the uranium in uraniferous sandstones mainly exists in two occurrence forms of uranium minerals and adsorbed uranium and that the proportion of minerals is significantly higher than that of adsorbed uranium. The contents of carbonate-bound uranium and organic-pyrite-bound uranium in medium- and high-grade samples increased notably. The formation of the Pengyang uranium deposit is closely related to the participation of reducing fluids such as oil and gas. The types and symbiotic relationships of altered minerals in the deposit indicate that ore-bearing sandstones have experienced a variety of fluid activities. Numerous alteration minerals, including anatase, pyrite, apatite, and clay minerals, in the uraniferous sandstone have played various roles in the complex mineralization process of adsorption, catalysis, reduction, and precipitation. In-situ S isotope of the colloidal pyrite shows that the biological process is of great significance to the enrichment and precipitation of colloidal pyrite and uranium. These may be the important mechanisms of uranium precipitation and enrichment.
英文关键词Uranium occurrence state Enrichment mechanism Sandstone-type uranium deposit Luohe Formation Ordos Basin
类型Article
语种英语
开放获取类型hybrid
收录类别SCI-E
WOS记录号WOS:000747580800001
WOS关键词CARBONIFEROUS BLACK SHALE ; ORE-FORMING PROCESSES ; CRETACEOUS DESERT ; ERLIAN BASIN ; SANDSTONE ; GENESIS ; REDUCTION ; CHINA ; PYRITE ; BIOMINERALIZATION
WOS类目Geology ; Mineralogy ; Mining & Mineral Processing
WOS研究方向Geology ; Mineralogy ; Mining & Mineral Processing
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/376903
作者单位[Zhao, Hualei; Ao, Cong; Chen, Lulu; Zhang, Bo; Miao, Peisen; Zhu, Qiang; Yu, Rengan; Chen, Yin] China Geol Survey, Tianjin Ctr, Tianjin 300170, Peoples R China; [Zhao, Hualei; Ao, Cong; Li, Jianguo; Chen, Lulu; Zhang, Bo; Si, Qinghong; Zhu, Qiang; Yu, Rengan; Chen, Yin] China Geol Survey, Key Lab Uranium Geol, Tianjin 300170, Peoples R China; [Li, Jianguo] China Geol Survey, Cores & Samples Ctr Nat Resources, Beijing 100192, Peoples R China
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GB/T 7714
Zhao, Hualei,Ao, Cong,Li, Jianguo,et al. Occurrence and mechanism of uranium enrichment with a unique eolian sedimental environment in the Pengyang uranium deposit, Ordos Basin[J],2022,141.
APA Zhao, Hualei.,Ao, Cong.,Li, Jianguo.,Chen, Lulu.,Zhang, Bo.,...&Chen, Yin.(2022).Occurrence and mechanism of uranium enrichment with a unique eolian sedimental environment in the Pengyang uranium deposit, Ordos Basin.ORE GEOLOGY REVIEWS,141.
MLA Zhao, Hualei,et al."Occurrence and mechanism of uranium enrichment with a unique eolian sedimental environment in the Pengyang uranium deposit, Ordos Basin".ORE GEOLOGY REVIEWS 141(2022).
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