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    Volume 50 Issue 6
    Jun.  2025
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    Article Contents
    Yu Xiaoliang, Li Hua, Wei Xiaolin, Zhang Huiqing, Li Jie, Gu Chao, Tong Haikui, Chen Huayong, Xiao Bing, Wang Hao, Zhang Binshun, 2025. Zircon U-Pb Age and Geochemical Characteristics of Granitic Magmatic Rocks in Mailong Gold Deposit, East Kunlun, and Their Geological Significance. Earth Science, 50(6): 2107-2123. doi: 10.3799/dqkx.2025.046
    Citation: Yu Xiaoliang, Li Hua, Wei Xiaolin, Zhang Huiqing, Li Jie, Gu Chao, Tong Haikui, Chen Huayong, Xiao Bing, Wang Hao, Zhang Binshun, 2025. Zircon U-Pb Age and Geochemical Characteristics of Granitic Magmatic Rocks in Mailong Gold Deposit, East Kunlun, and Their Geological Significance. Earth Science, 50(6): 2107-2123. doi: 10.3799/dqkx.2025.046

    Zircon U-Pb Age and Geochemical Characteristics of Granitic Magmatic Rocks in Mailong Gold Deposit, East Kunlun, and Their Geological Significance

    doi: 10.3799/dqkx.2025.046
    • Received Date: 2024-05-22
    • Publish Date: 2025-06-25
    • To reveal the tectonic evolution of the Proto-Tethys and Paleo-Tethys Oceans and their genetic links to gold-polymetallic mineralization in the East Kunlun orogenic belt (EKOB), this study conducted petrographic, geochemical, and LA-ICP-MS zircon U-Pb geochronological analyses on monzogranite and granodiorite from the Mailong gold deposit. The results show that the monzogranite and granodiorite crystallized at 421±11 Ma (Late Silurian) and 228±4 Ma (Late Triassic), respectively, exhibiting metaluminous, high-potassium calc-alkaline characteristics. Trace element analyses reveal enrichment in light rare earth elements (LREE), large-ion lithophile elements (LILE: Rb, K), and incompatible elements (U, Th, Pb), with depletion in high-field-strength elements (HFSE: Nb, Ta, P, Ti) and weak negative Eu anomalies, indicating an island arc granite affinity. Combined with regional geological evidence, these rocks formed through crust-mantle interaction during the post-orogenic extensional stage. The Mailong gold deposit, primarily hosted in the granodiorite, is likely associated with tectonic-magmatic activities during the post-orogenic extension of the Paleo-Tethys evolution. This study provides critical age constraints and geochemical insights into the tectonic evolution and gold mineralization in the EKOB, offering valuable guidance for regional mineral exploration.

       

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