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    中国百强科技报刊

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    Volume 47 Issue 10
    Oct.  2022
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    Article Contents
    Jiao Yangquan, Wu Liqun, Rong Hui, Zhang Fan, Yue Liang, Song Hao, Tao Zhenpeng, Peng Hu, Sun Yuhan, Xiang Yao, 2022. Sedimentation, Diagenesis and Uranium Mineralization: Innovative Discoveries and Cognitive Challenges in Study of Sandstone-Type Uranium Deposits in China. Earth Science, 47(10): 3580-3602. doi: 10.3799/dqkx.2022.284
    Citation: Jiao Yangquan, Wu Liqun, Rong Hui, Zhang Fan, Yue Liang, Song Hao, Tao Zhenpeng, Peng Hu, Sun Yuhan, Xiang Yao, 2022. Sedimentation, Diagenesis and Uranium Mineralization: Innovative Discoveries and Cognitive Challenges in Study of Sandstone-Type Uranium Deposits in China. Earth Science, 47(10): 3580-3602. doi: 10.3799/dqkx.2022.284

    Sedimentation, Diagenesis and Uranium Mineralization: Innovative Discoveries and Cognitive Challenges in Study of Sandstone-Type Uranium Deposits in China

    doi: 10.3799/dqkx.2022.284
    • Received Date: 2022-04-23
    • Publish Date: 2022-10-25
    • In the 21th century, China has made brilliant achievements in the exploration of sandstone-type uranium deposits. Sandstone-type uranium deposits are located in sedimentary basins. The formation of uranium deposits must go through two important evolutionary stages from sedimentary burial stage to uplift metallogenic stage. The participation and restriction of atmospheric precipitation and oxidation-reduction are the most significant metallogenic characteristics in the uplift metallogenic stage. Obviously, this is the product of a typical supergene diagenesis, an important link in the complex diagenetic sequence of uranium reservoirs, and belongs to the category of "exogenetic mineralization". Although the mineralization of sandstone-type uranium deposit follows the general mechanism of oxidation-reduction and uranium valence change, the special sedimentary background leads to the diversity and regional specificity of uranium mineralization. Some key ore controlling elements created by sedimentation, sedimentary environment and paleoclimate can directly affect uranium mineralization in epigenetic rock stage from "gene". From sedimentation, diagenesis to uranium mineralization is a geological process with genetic connection, and the basin-mountain coupling mechanism is always the most fundamental original driving force. With the in-depth study of the detailed behavior of uranium mineralization, some innovative discoveries continue to impact the previous inherent understanding, such as the interaction between carbonaceous debris and uranium mineralization, the complex and orderly evolution habit of pyrite, the symbiosis and superposition of carbonate cement and uranium mineralization, the fluid tracing of sensitive minerals, the uranium mineralization mechanism restricted by the heterogeneity of uranium reservoir, the ore making model of double reducing medium, and compound geochemical barrier of uranium mineralization, etc. Other studies have posed cognitive challenges to traditional geological theories, such as the "carbonization mechanism" of carbonaceous debris in the open diagenetic environment of uranium reservoir, the chemical dynamic mechanism of uranium precipitation on the dissolution or growth interfaces of pyrite, the uranium metallogenic mechanism in arid sedimentary background, etc. At the same time, the study of uranium metallogenic mechanism and general law has also laid a good geological foundation for the study of geological effects of sandstone-type uranium deposit decay and the systematic exploration of basin uranium resources. It is believed that the systematic study on the metallogenic mechanism and genetic relationship of the whole sedimentary basin will release the huge basin uranium resource potential and deposit productivity, and help to achieve the "double carbon goal" while further enriching the uranium metallogenic theory.

       

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