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    Volume 48 Issue 11
    Nov.  2023
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    Article Navigation >  Earth Science  > 2023  >  48(11): 4214-4228
    Lin Xu, Li Lingling, Liu Jing, Wu Zhonghai, Li Chang'an, Liu Weiming, Xiang Yu, Liu Haijin, Chen Jixin, 2023. Yangtze River Contributed Detrital Materials to Jianghan Basin during Early Pleistocene: Constraints from Detrital Zircon U-Pb Ages. Earth Science, 48(11): 4214-4228. doi: 10.3799/dqkx.2022.018
    Citation: Lin Xu, Li Lingling, Liu Jing, Wu Zhonghai, Li Chang'an, Liu Weiming, Xiang Yu, Liu Haijin, Chen Jixin, 2023. Yangtze River Contributed Detrital Materials to Jianghan Basin during Early Pleistocene: Constraints from Detrital Zircon U-Pb Ages. Earth Science, 48(11): 4214-4228. doi: 10.3799/dqkx.2022.018
    shu

    Yangtze River Contributed Detrital Materials to Jianghan Basin during Early Pleistocene: Constraints from Detrital Zircon U-Pb Ages

    doi: 10.3799/dqkx.2022.018
    • 1.

      School of Civil Engineering and Architecture, China Three Gorges University, Yichang 443002, China

    • 2.

      Key Laboratory of Geological Hazards in Three Gorges Reservoir Area, Ministry of Education, China Three Gorges University, Yichang 443002, China

    • 3.

      School of Earth System Science, Tianjin University, Tianjin 300072, China

    • 4.

      Key Laboratory of Neotectonic Movement and Geohazards, Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China

    • 5.

      School of Geography and Information Engineering, China University of Geosciences, Wuhan 430078, China

    • 6.

      Institute of Mountain Hazards and Environment, Chinese Academy of Sciences and Ministry of Water Resources, Chengdu 610041, China

    • 7.

      School of Geography Science, Fujian Normal University, Fuzhou 350007, China

    • 8.

      School of Earth Sciences, East China University of Technology, Nanchang 330013, China

    • Received Date: 2021-10-13
      Available Online: 2023-11-30
    • Publish Date: 2023-11-25
      Abstract
    • It remains controversial whether the Yichang and Yangluo gravel beds in the west and east of the Jianghan basin are related to the evolution and development of the Yangtze River. To address the problem, it carried out the detrital zircon U-Pb age analysis from the Yichang and Yangluo gravel layers. The U-Pb age analysis was also conducted on the Juzhang and Qingjiang rivers close to the Yichang gravel layers. It also analyzes detrital zircon U-Pb ages in Huanshui, Daoshui and Jushui rivers surrounding the Yangluo gravel bed. A total of 654 new zircon U-Pb ages have been reported. It collected the published detrital zircon U-Pb ages from the upper reach of the Yangtze River in the region, combined with the sedimentary age of the gravel beds, and systematically identified the material sources of the Yichang and Yangluo gravel beds. The results show that the Yangtze River becomes the sand material supply river of Yichang and Yangluo gravel beds in 1.2-0.7 Ma and 1.3 Ma, respectively. The comparison with the gravel beds in the upper and lower reaches of the Yangtze River and the provenance tracing results indicate that the Yangtze River appeared in the Early Pleistocene in response to the uplift of the Tibetan plateau and the intensification of the East Asian summer monsoon. Therefore, the combination of continuous tectonic processes and environmental changes in East Asia during the Early Pleistocene was crucial to the stable emergence of the Yangtze River with a continent-scale length of more than 6 000 km.

       

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