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Wang, Qiang; Wang, Yong; Wang, Xueqiu; Cheng, Zhizhong; Jiang, Xiaojun; Liu, Hanliang; Tian, Mi; Wang, Dongsheng (2025) Characterization of primary geochemical halos for the Hetaoba volcanic-related uranium deposits in Duolun County, Inner Mongolia. Ore Geology Reviews, 181. 106611 doi:10.1016/j.oregeorev.2025.106611

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Reference Type	Journal (article/letter/editorial)
Title	Characterization of primary geochemical halos for the Hetaoba volcanic-related uranium deposits in Duolun County, Inner Mongolia
Journal	Ore Geology Reviews
Authors	Wang, Qiang		Author
	Wang, Yong		Author
	Wang, Xueqiu		Author
	Cheng, Zhizhong		Author
	Jiang, Xiaojun		Author
	Liu, Hanliang		Author
	Tian, Mi		Author
	Wang, Dongsheng		Author
Year	2025	Volume	< 181 >
Page(s)	106611
URL	https://www.sciencedirect.com/science/article/pii/S0169136825001714
DOI	doi:10.1016/j.oregeorev.2025.106611Search in ResearchGate
	Generate Citation Formats
Classification	Not set	LoC	Not set
Mindat Ref. ID	18271192	Long-form Identifier	mindat:1:5:18271192:7
GUID	0
Full Reference	Wang, Qiang; Wang, Yong; Wang, Xueqiu; Cheng, Zhizhong; Jiang, Xiaojun; Liu, Hanliang; Tian, Mi; Wang, Dongsheng (2025) Characterization of primary geochemical halos for the Hetaoba volcanic-related uranium deposits in Duolun County, Inner Mongolia. Ore Geology Reviews, 181. 106611 doi:10.1016/j.oregeorev.2025.106611
Plain Text	Wang, Qiang; Wang, Yong; Wang, Xueqiu; Cheng, Zhizhong; Jiang, Xiaojun; Liu, Hanliang; Tian, Mi; Wang, Dongsheng (2025) Characterization of primary geochemical halos for the Hetaoba volcanic-related uranium deposits in Duolun County, Inner Mongolia. Ore Geology Reviews, 181. 106611 doi:10.1016/j.oregeorev.2025.106611
In	Link this record to the correct parent record (if possible)
Abstract/Notes	Primary geochemical halo is a powerful tool for exploring blind deposits. However, primary geochemical halo studies have seldom been conducted on hydrothermal uranium deposits. This study conducted primary geochemical halo studies on the Hetaoba volcanic-related uranium deposit in the Guyuan–Hongshanzi uranium-polymetallic metallogenic belt based on the 780 core samples with 20 elements analyzed from 13 boreholes. Staged factor analysis (SFA) of the centered log-ratio (CLR) transformed data showed that an ore-related elemental association is F1 (U–Mo–As–Pb–Cd–Sb association). However, scatter plots and anomaly maps based on the thresholds determined by the concentration–number (C–N) fractal model showed that the extent of sulfide-rich zones was larger than that of uranium mineralization, and some sulfide-rich zones were accompanied by low uranium content, although uranium mineralization was always accompanied by sulfide enrichment. Furthermore, uranium minerals were distributed along the metal sulfide edges and even encased them, suggesting that uranium mineralization may have occurred later than the sulfide precipitation. Zoning patterns of indicator elements (from top to bottom) for ore bodies at shallow (AZS1) and greater (AZS2) depths determined by Gregorian’s method are Bi–Zn–Cd–Mo–Sb–Cs–Pb–Hg–U–Sc–Be–Li–W–Cu–As–Tl–V–Co–Cr–Ni and Cr–Ni–Sc–Be–W–V–Co–Sb–As–Bi–Cu–Pb–Mo–U–Hg–Zn–Cd–Li–Tl–Cs, respectively. These results are significant for mineral exploration. Sulfide-rich zones may provide favorable space and reducing agents for uranium mineralization and can serve as an auxiliary indicator for uranium exploration. More importantly, strong Hg anomalies at relatively greater depths may represent favorable traps for uranium deposition. Consequently, Hg can serve as a near-ore indicator of uranium exploration at relatively greater depths. In addition, AZS2 front-halo elements may suggest the superposition of two metallogenetic stages and exploration potential in the up-dip of the fault zone.

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👁 Image	Zuo, Renguang (2014) Identification of geochemical anomalies associated with mineralization in the Fanshan district, Fujian, China. Journal of Geochemical Exploration, 139. 170-176 doi:10.1016/j.gexplo.2013.08.013

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Locality	Citation Details
Hetaoba U deposit, Duolun County, Xilingol League (Xilinguole Prefecture), Inner Mongolia, China

Mineral Occurrences

Locality	Mineral(s)
Hetaoba U deposit, Duolun County, Xilingol League (Xilinguole Prefecture), Inner Mongolia, China	ⓘ Apatite, ⓘ Chlorite Group, ⓘ Feldspar Group, ⓘ Fluorite, ⓘ Galena, ⓘ Granite, ⓘ Hematite, ⓘ Molybdenite, ⓘ Porphyry, ⓘ Pyrite, ⓘ Quartz, ⓘ Rhyolite, ⓘ Sphalerite, ⓘ Uraninite

URL: https://www.mindat.org/reference.php?id=18271192

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