松辽盆地西南部含铀岩系沉积时的古气候演变及其与铀成矿关系

江文剑; 秦明宽; 范洪海; 贾立城; 郭强; 黄少华; 宁君; 肖菁

doi:10.3799/dqkx.2022.388

Volume 48 Issue 3

Mar. 2023

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Article Navigation > Earth Science > 2023 > 48(3): 1232-1245

Jiang Wenjian, Qin Mingkuan, Fan Honghai, Jia Licheng, Guo Qiang, Huang Shaohua, Ning Jun, Xiao Jing, 2023. Paleoclimate Evolution and Uranium Mineralization during the Deposition of Uranium-Bearing Rocks in the Southwest of Songliao Basin. Earth Science, 48(3): 1232-1245. doi: 10.3799/dqkx.2022.388

Citation:

Jiang Wenjian, Qin Mingkuan, Fan Honghai, Jia Licheng, Guo Qiang, Huang Shaohua, Ning Jun, Xiao Jing, 2023. Paleoclimate Evolution and Uranium Mineralization during the Deposition of Uranium-Bearing Rocks in the Southwest of Songliao Basin. Earth Science, 48(3): 1232-1245. doi: 10.3799/dqkx.2022.388

Citation:

Jiang Wenjian, Qin Mingkuan, Fan Honghai, Jia Licheng, Guo Qiang, Huang Shaohua, Ning Jun, Xiao Jing, 2023. Paleoclimate Evolution and Uranium Mineralization during the Deposition of Uranium-Bearing Rocks in the Southwest of Songliao Basin. Earth Science, 48(3): 1232-1245. doi: 10.3799/dqkx.2022.388

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Paleoclimate Evolution and Uranium Mineralization during the Deposition of Uranium-Bearing Rocks in the Southwest of Songliao Basin

doi: 10.3799/dqkx.2022.388

1.
CNNC Key Laboratory of Uranium Resource Exploration and Evaluation Technology, Beijing Research Institute of Uranium Geology, Beijing 100029, China
2.
State Key Laboratory of Nuclear Resources and Environment, East China University of Technology, Nanchang 330013, China
3.
Geological Party No.243, CNNC, Chifeng 024006, China

Received Date: 2022-04-20
Available Online: 2023-03-27
Publish Date: 2023-03-25

Abstract

Abstract

Although, the paleoclimate plays an important role in controlling uranium mineralization during the deposition of uranium-bearing rocks, it has not attracted enough attention of uranium geologists for a long time. The lower member of Yaojia formation is the ore bearing target layer in the southwest of Songliao basin. Taking the lower member of Yaojia formation as the research object, the contents of the main and trace elements and total organic carbon of mudstone samples from representative boreholes were tested. A number of chemical weathering indexes, such as K/Na ratio, a^AlNa, chemical proxy of alteration (CPA), modified chemical index of alteration (CIX), plagioclase index of alteration (PIA), chemical index of weathering (CIW), chemical index of alteration (CIA), are used to judge the intensity of chemical weathering of the samples, and reconstruct the paleoclimate conditions during the depositional period. At the same time, combined with the contents of U and TOC and the ratio of Fe²⁺/Fe³⁺, the constraints of paleoclimate conditions on uranium mineralization during the deposition of uranium-bearing rock series in the study area are discussed. The results show that the clastic rocks in the study area have experienced the change of chemical weathering intensity from weak to strong to weak, indicating that the evolution law of paleoclimate from relative cold and drought to relative warm and humidity to relative cold and drought. This paleoclimate change leads to low TOC content in uranium reservoir sand bodies (average value 0.05%) and large-scale development of interlayer oxidation zone, so uranium ore bodies are mainly located in the hinterland of the basin far away from the erosion source area. Dark mudstone formed in humid climate has higher TOC (average 0.61%) and U content (up to 885×10^-6). It has become one of the important sources of uranium due to its strong preconcentration during deposition. The discharge of reducing pore water during diagenesis may be the main factor for the construction of oxidation-reduction barrier in uranium reservoir sand bodies. During deposition, the warm and humid climate enhances the intensity of chemical weathering in the source area, which is conducive to the activation and leaching of uranium in the parent rock and the uranium preconcentration of mudstone in the sedimentary area.
- chemical weathering,
- paleoclimate,
- sandstone-type uranium deposit,
- uranium mineralization,
- Yaojia Formation,
- Songliao basin,
- mineral deposits

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References(62)

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Paleoclimate Evolution and Uranium Mineralization during the Deposition of Uranium-Bearing Rocks in the Southwest of Songliao Basin

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