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    中国百强科技报刊

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    Volume 46 Issue 10
    Nov.  2021
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    Article Contents
    Li Lushun, Wang Zecheng, Xiao Ancheng, Yang Gaoyin, Jiang Hua, Su Nan, Wu Lei, Shi Pingping, Wang Yiping, 2021. Rift System in Northern Yangtze Block during Nanhua Period: Implications from Gravity Anomaly and Sedimentology. Earth Science, 46(10): 3496-3508. doi: 10.3799/dqkx.2020.395
    Citation: Li Lushun, Wang Zecheng, Xiao Ancheng, Yang Gaoyin, Jiang Hua, Su Nan, Wu Lei, Shi Pingping, Wang Yiping, 2021. Rift System in Northern Yangtze Block during Nanhua Period: Implications from Gravity Anomaly and Sedimentology. Earth Science, 46(10): 3496-3508. doi: 10.3799/dqkx.2020.395

    Rift System in Northern Yangtze Block during Nanhua Period: Implications from Gravity Anomaly and Sedimentology

    doi: 10.3799/dqkx.2020.395
    • Received Date: 2020-12-26
      Available Online: 2021-11-03
    • Publish Date: 2021-11-03
    • A series of rift valleys and their related sedimentary basins were developed in South China during Nanhua period. There are direct evidences of rift valleys in Kangdian area, Sichuan basin and Hunan-Guangxi area. However, there is no clear understanding of the existence of rift basin due to the complex terrain and weak previous studies in the Daba Mountain area. The study of this area is helpful to understand the existence of Nanhua rift in Daba Mountain area and provides some enlightenment for the study of tectonic evolution in northern Yangtze block.In this paper, the gravity anomaly and field outcrop data were used to carry out a comprehensive study in this area. The present distribution pattern of Nanhua rift was revealed in Daba Mountain area, northern Yangtze block, and the stratigraphic filling sequence and spatial framework in and between the rifts were constructed. The study shows that the Daba Mountain rift is east-west trending along Zhushan-Dazhou, extending from the middle of South Qinling to the northeast of Sichuan basin. Based on the basin framework and sedimentary filling characteristics, the tectonic background of the back-arc rift in the Daba Mountain area is proposed, which provides enlightenment for the Neoproterozoic dynamic mechanism in the northern margin of the Yangtze block.

       

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