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2023 Vol. 50, No. 5
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Article navigation > Geology in China > 2023 > 50(5): 1327-1342
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ZHANG Chao, SI Qinghong, YU Reng'an, WANG Shanbo, CHENG Yinhang, YU Hang, FENG Ping, SHI Guangshun, AO Cong, LI Zhidan, GAO Xuefeng. 2023. Analysis of the relationship between sedimentary characteristics and uranium deposits from the Neogene Shizigou Formation in Huatugou area, Northwest Qaidam Basin[J]. Geology in China, 50(5): 1327-1342. doi: 10.12029/gc20200720004
Citation: ZHANG Chao, SI Qinghong, YU Reng'an, WANG Shanbo, CHENG Yinhang, YU Hang, FENG Ping, SHI Guangshun, AO Cong, LI Zhidan, GAO Xuefeng. 2023. Analysis of the relationship between sedimentary characteristics and uranium deposits from the Neogene Shizigou Formation in Huatugou area, Northwest Qaidam Basin[J]. Geology in China, 50(5): 1327-1342. doi: 10.12029/gc20200720004
shu

Analysis of the relationship between sedimentary characteristics and uranium deposits from the Neogene Shizigou Formation in Huatugou area, Northwest Qaidam Basin

  • 1.

    Tianjin Center, China Geological Survey, Tianjin 300170, China

  • 2.

    Key Laboratory of Uranium Geology of China Geological Survey, Tianjin 300170, China

  • 3.

    The Nuclear Industry Geological Survey 283 Brigade in Sichuan Province, Dazhou 635000, Sichuan, China

  • 4.

    Shandong Provincial Architecture Design and Research Institute, Jinan 250002, Shandong, China

  • 5.

    PetroChina Qinghai Oilfield Company, Dunhuang 736200, Gansu, China

    • Fund Project: Supported by the projects of China Geological Survey (No.DD20190119) and National Key R&D Program of China (No.2018YFC0604200)
More Information
  • Author Bio: ZHANG Chao, male, born in 1987, master, senior engineer, engaged in the study of sedimentary geochemistry, mineralogy and the geological survey of mineral resources; E-mail: 402709002@qq.com
Received Date:  20 July 2020
Revised Date:  01 October 2020
Publish Date:  25 October 2023
    Abstract

  • This paper is the result of mineral exploration engineering.

     Objective

    Typical sandstone type uranium deposits are developed in Huatugou area, Northwest Qaidam Basin. The uranium reservoirs are Qigequan Formation, Shizigou Formation and Youshashan Formation, while Shizigou Formation is somewhere in between Qigequan Formation and Youshashan Formation. It is an urgent geological problem to correctly understand the relationship between sedimentary characteristics of Shizigou Formation and sandstone-type uranium deposits.

     Methods

    In this paper, the sedimentary characteristics of Shizigou Formation are studied based on the sandstone-type uranium deposit prospecting work in the Qaidam Basin, and we analyzed the stratigraphic sequence frame, cause mechanism, provenance characteristics and their relationship with uranium ore from Shizigou Formation.

     Results

    The colour of greywacke collected from ZK10 in Yuejin 2 area is brownish red, while the main body is calcareous argillaceous sandstone, which belongs to carbonate terrigenous clastic greywacke. Specific value of CIA=37.79-69.14, ICV=0.84-2.13, Σ=1.39-2.14, K2O/Na2O=0.90-1.18 (the average is 1.06), which indicated that there are relatively much more potassium feldspar or potassium minerals in the greywacke. The measuring result from a depth of 224 to 240 meter is GR=0-30 API, RT=-5-45 Ω·m. The logging facies is box type, and the amplitude of the curve is large. The measuring result of greywacke is K2O/Al2O3=0.22-0.27, Ni/Co=0.34-0.53.

     Conclusions

    The sediment environment of Shizigou Formation in Yuejin 2 area belongs to fluvial facies. The source rocks of the upper Shizigou Formation contain less clay material, and were deposited for the first time under the dry and cold paleoclimate environment. The source rock of greywacke in the Shizigou Formation were formed in the continental island arc environment, which the sedimentary source rock of the greywacke is the alkali feldspar with a small amount of felsic rocks. The sedimentary environment of the formation is very conducive for the formation of uranium deposits.
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