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2021 Vol. 48, No. 2
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HUANG Guangwen, YU Fucheng, PAN Jiayong, CHENG Zhengle, WU Dehai, XUE Wanwen, SONG Taizhong, LI Shanping. 2021. Genesis of pyrite from the Mengqiguer uranium deposit in Ili Basin of Xinjiang and its implication for mineralization[J]. Geology in China, 48(2): 507-519. doi: 10.12029/gc20210211
Citation: HUANG Guangwen, YU Fucheng, PAN Jiayong, CHENG Zhengle, WU Dehai, XUE Wanwen, SONG Taizhong, LI Shanping. 2021. Genesis of pyrite from the Mengqiguer uranium deposit in Ili Basin of Xinjiang and its implication for mineralization[J]. Geology in China, 48(2): 507-519. doi: 10.12029/gc20210211
shu

Genesis of pyrite from the Mengqiguer uranium deposit in Ili Basin of Xinjiang and its implication for mineralization

  • 1.

    State Key Laboratory of Nuclear Resources and Environment, East China University of Technology, Nanchang 330013, Jiangxi, China

  • 2.

    Qinghai Province Key Laboratory of Geological Process and Mineral Resources of Northern Qinghai-Tibet Plateau, Qinghai Geological Survey Institute, Xining 810012, Qinghai, China

  • 3.

    Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China

    • Fund Project: Supported by National Natural Science Foundation of China(No. 41772066, No.41902075, No.42002095), Key Laboratory of the Northern Qinghai-Tibet Plateau Geological Processes and Mineral Resources (No. 2019-KY-04), the Natural Science Foundation of Qinghai Provincial Department of Science and Technology (No. 2018-SF-109, No. 2019-ZJ-955Q), Qinghai-Tibet Plateau secondary research (No. 2019QZKK0702) and Postgraduate Innovation Fund Project of Jiangxi Province, China (No. YC2018-B082)
More Information
  • Author Bio: HUANG Guangwen, male, born in 1991, doctoral candidate, majoring in the exploration and research of uranium geology; E-mail: 807334699@qq.com
  • Corresponding author: PAN Jiayong, male, born in 1967, professor, supervisor of doctor candidates, engaged in the teaching and research of deposit geochemistry; E-mail: jypan@ecit.cn 
Received Date:  17 October 2019
Revised Date:  28 December 2019
Publish Date:  25 April 2021
    Abstract

  • The Mengqiguer uranium deposit in the Ili Basin is the largest sandstone-hosted one discovered in recent years. In order to research the source of ore-forming materials, the properties of ore-forming fluids and the metallogenic environment of the deposit, a geochemical studies on trace elements and sulfur isotope of the pyrites (the gangue minerals in Xishanyao Formation and Badaowan Formation, which closely related to ore minerals such as uraninite and coffinite) were carried out systematically. The results show that the REEs of pyrite in each sample exhibits a similar distribution pattern, that is, LREE is significantly more enriched than HREE (LaN/YbN=4.27-9.82), with strong negative Eu anomaly (δEu=0.50-0.71) and no Ce anomaly (δCe=0.93-1.04).The Co contents of pyrite range from 2.1×10-6 to 26.7×10-6, Ni from 19.5×10-6 to 79.30×10-6, the ratio of Co/Ni from 0.07 to 0.88, and As from 8.90×10-6 to 95.60×10-6 higher than the average As content of the continental crust. The sulfur isotope composition of pyrite has a relatively wide range of variation, i.e. δ34SCDT ranging from -17.30‰ to 3.90‰, with the change range of 21.20‰. Combined with characteristics of REEs, trace elements and sulfur isotope composition of pyrites and regional metallogenic setting, it is suggested that pyrite in this deposit is of sedimentary origin and was formed in a low temperature reduction environment. It is concluded that the sulfur of pyrite mainly originates from coal and sedimentary sulfide with microbial genetic characteristics, and pyrites and charcoal debris (organic matters) provide reductants for redox reactions during uranium mineralization.

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