Arid
DOI10.1016/j.gexplo.2021.106797
Source identification of the geochemical anomaly from the fine-grained soil survey in the Nuheting sandstone-type uranium deposit, Erlian Basin, north China
Lu, Mei; Ye, Rong; Zhang, Bimin
通讯作者Ye, R (corresponding author), China Univ Geosci, Sch Earth Sci & Resources, Beijing 100083, Peoples R China. ; Zhang, BM (corresponding author), Inst Geophys & Geochem Explorat, Key Lab Geochem Explorat, Langfang 06500, Peoples R China.
来源期刊JOURNAL OF GEOCHEMICAL EXPLORATION
ISSN0375-6742
EISSN1879-1689
出版年2021
卷号227
英文摘要Sedimentary basins in the arid areas of northern China have great potential to aid the discovery of new sandstone-type uranium deposits. A fine-grained (<75 mu m) soil survey covering an area of approximately 6400 km2 has been undertaken to explore the concealed sandstone-type uranium deposit in Erlian Basin, north China. Displaying an obvious geochemical anomaly, the Nuheting (NHT) sandstone-type uranium deposit has been chosen for detailed studies of the source of geochemical anomaly, using lead (Pb) isotopic tracing and nanoparticle observation. Fine-grained soils are divided into three groups according to their spatial distance to the NHT uranium deposit which are soils above deposit, proximal soils and distal soils. Using analysis of variance (ANOVA), Pb isotope ratios of these soils show significant difference between proximal and distal samples. Deep mineralization and regional faults may give rise to the difference of radiogenic Pb isotopes. In addition, the widely observed Mo-bearing nanoparticles provide evidence that fine-grained soils contain signature of deep uranium ore. The characteristics of Pb isotope and nanoparticles indicate that accumulation of radiogenic Pb isotopes in the fine-grained soils is resulted from the concealed NHT uranium deposit. The transport and evaporation of groundwater has led to the vertical migration of geochemical signature from the deep to the surface. The fine-grained soil survey shows promise as an effective exploration technique for the sandstone-type uranium deposit in arid areas.
英文关键词Fine-grained soil survey Geochemical anomaly Lead isotope Nanoparticle Sandstone-type uranium deposit
类型Article
语种英语
收录类别SCI-E
WOS记录号WOS:000663433000002
WOS关键词ASCENDING GAS-FLOW ; MINERAL EXPLORATION ; SEDIMENTARY-ROCKS ; DESERT REGOLITH ; GOLD ; LEAD ; NANOPARTICLES ; PARTICLES ; COVER ; TEM
WOS类目Geochemistry & Geophysics
WOS研究方向Geochemistry & Geophysics
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/350826
作者单位[Lu, Mei; Ye, Rong] China Univ Geosci, Sch Earth Sci & Resources, Beijing 100083, Peoples R China; [Lu, Mei] Chinese Acad Sci, Guangzhou Inst Geochem, CAS Key Lab Mineral & Metallogeny, Guangdong Prov Key Lab Mineral Phys & Mat, Guangzhou 510640, Peoples R China; [Lu, Mei] CAS Ctr Excellence Deep Earth Sci, Guangzhou 510640, Peoples R China; [Zhang, Bimin] Inst Geophys & Geochem Explorat, Key Lab Geochem Explorat, Langfang 06500, Peoples R China; [Zhang, Bimin] UNESCO Int Ctr Global Scale Geochem, Langfang 065000, Peoples R China
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GB/T 7714
Lu, Mei,Ye, Rong,Zhang, Bimin. Source identification of the geochemical anomaly from the fine-grained soil survey in the Nuheting sandstone-type uranium deposit, Erlian Basin, north China[J],2021,227.
APA Lu, Mei,Ye, Rong,&Zhang, Bimin.(2021).Source identification of the geochemical anomaly from the fine-grained soil survey in the Nuheting sandstone-type uranium deposit, Erlian Basin, north China.JOURNAL OF GEOCHEMICAL EXPLORATION,227.
MLA Lu, Mei,et al."Source identification of the geochemical anomaly from the fine-grained soil survey in the Nuheting sandstone-type uranium deposit, Erlian Basin, north China".JOURNAL OF GEOCHEMICAL EXPLORATION 227(2021).
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