Journal of Jilin University(Earth Science Edition) ›› 2018, Vol. 48 ›› Issue (1): 165-180.doi: 10.13278/j.cnki.jjuese.20160232

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A SHRIMP U-Pb Zircon Geochronology of a Tuff Bed from the Bottom of Liantuo Formation in the Three Gorges Area and Its Geological Implications

Jing Xianqing1, Yang Zhenyu2, Tong Yabo3, Wang Heng4, Xu Yingchao5   

  1. 1. School of Earth Sciences and Engineering, Nanjing University, Nanjing 210093, China;
    2. College of Geospatial Information Science and Technology, Capital Normal University, Beijing 100048, China;
    3. Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China;
    4. Institute of Geology, China Earthquake Administration, Beijing 100029, China;
    5. School of Earth Sciences, China University of Geosciences, Wuhan 430074, China
  • Received:2016-09-12 Online:2018-01-26 Published:2018-01-26
  • Supported by:
    Supported by National Natural Science Foundation of China (41230208)

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Abstract: The Mid-late Neoproterozoic strata in the Three Gorges area may record a series drastic changes on the earth system. Although the Liantuo Formation may experience the breakup of the Rodinia and the start age of the Nanhuan glaciation, its age and regional stratigraphic correlation are controversial. In this study, we obtained two SHRIMP U-Pb age of (810±7) Ma and (763±10) Ma from a tuff bed in the bottom of the Liantuo Formation. The older one may represent the resedimentation of the Huangling granites. Together with the reported ages, we suggest that the Liantuo Formation in the Three Gorges area was deposited during 780-714 Ma. The regional stratigraphic correlation suggests that the Liantuo Formation is related to Chengjing/Kaijianqiao Formation and the Banxi, Xiajiang and Danzhou Group. Whereas, due to the lack of the early stage deposition (820-790 Ma), the Liantuo Formation can be related only to the mid-upper part of the Xiajiang Group and Danzhou Group.

Key words: Liantuo Formation, tuff, SHRIMP U-Pb zircon geochronology, regional correlation, Three Gorges area

CLC Number: 

  • P588.1
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