Journal of Jilin University(Earth Science Edition) ›› 2018, Vol. 48 ›› Issue (6): 1609-1624.doi: 10.13278/j.cnki.jjuese.20170184

   

Cambrian Sequence Stratigraphic Framework in Northern Margin of North China Craton

Wu Heyuan1,2,3, Zhao Zongju3, Wang Jianguo3, Wang Peixi3, Gong Faxiong4, Xiao Fei5   

  1. 1. School of Earth Sciences and Engineering, Xi'an Shiyou University, Xi'an 710065, China;
    2. Stdoctoral Workstation, Xinjiang Oilfield Company, PetroChina, Karamay 834000, Xinjiang, China;
    3. Chinese Petroleum Society, Beijing 100724, China;
    4. Research Institute of Exploration and Development, Jidong Oilfield Company, PetroChina, Tangshan 063004, Hebei, China;
    5. School of Energy Resources, China University of Geosciences, Beijing 100083, China
  • Received:2017-07-05 Published:2018-11-26
  • Supported by:
    Supported by Major National Science and Technology Projects (2011ZX05006) and PetroChina Jidong Oilfield Company (2013-JS-231)

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Abstract: Cambrian carbonate rocks are key targets for regional oil and gas exploration in the northern margin of the North China craton. The study of sedimentary environment and sequence stratigraphic framework is meaningful to stratigraphic correlating and reservoir locating, it can provide clues for the Cambrian oil and gas exploration in North China. Based on outcrop and core observation, thin section analysis, microscope interpretation and geochemical analysis, the lithology, lithofacies and the stack mode of strata were studied, and the sedimentary trend and the division of sequence stratigraphy were discussed. The authors consider that a massive transgression was happened from south to north after Proterozoic in the northern margin of the North China craton, which was controlled by global eustatic sea level changes. Under the double restriction of clastic supply and carbonatite accretion, the North China craton experienced an evolution process of carbonate platform from being built, developed to rimmed. Bordered by Zhangxia Formation, the Lower-Middle Cambrian performed as a gentle slope-shelf environment, while the Upper Cambrian was a rimmed platform. The Cambrian strata in the northern margin of North China can be divided into 7 third-order sequences with different types of boundaries, which are regionally correlated. The most high level system tracts always form a thick-layer carbonate rocks, which are the most important oil and gas reservoirs.

Key words: Cambrian, carbonate rocks, sequence stratigraphy, North China craton, cyclic stratigraphy

CLC Number: 

  • P618.13
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