Journal of Jilin University(Earth Science Edition) ›› 2019, Vol. 49 ›› Issue (5): 1222-1234.doi: 10.13278/j.cnki.jjuese.20180054

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Sedimentary Facies and Evolution of Upper Fourth Member of Paleogene Shahejie Formation in Western Sag of Liaohe Basin

Wang Xiabin1, Jiang Zaixing2, Hu Guangyi1, Fan Ting'en1, Wang Junhui3, Lu Huan4   

  1. 1. Research Institute Co., Ltd., CNOOC, Beijing 100028, China;
    2. School of Energy Resources, China University of Geosciences, Beijing 100083;
    3. College of Geosciences, China University of Petroleum, Beijing 102249, China;
    4. China Limited Tianjin Branch, CNOOC, Tianjin 300459, China
  • Received:2018-04-13 Published:2019-10-10
  • Supported by:
    Supported by Major Project of National Science and Technology (2017ZX05009-002)

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Abstract: The thin interbedded sand body is a difficult point in the study of lacustrine sedimentology. Based on the Fourth Member of the upper Shahejie Formation (Es4) in the Western sag of Liaohe basin, the theory of sequence stratigraphy, sedimentology and logging geology, the thin interbedded sand bodies are described and analyzed integrated with core, logging and seismic data. It is considered that the braided delta and lacustrine sedimentary facies are mainly developed in the study area, among which the beach bar is the main sand body. The beach bar can be divided into five different parts based on their different sedimentary genetic characteristics:the lateral reformed beach bar, the front reformed beach bar, the bedrock reformed beach bar, the flooded reformed beach bar,and the tempestite reformed beach bar. Through analysis of the control factors of the thin beach bar sand bodies,they are controlled by "wind field-source-basin".

Key words: Western sag of Liaohe basin, upper fourth member of Shahejie Formation, beach bar, sedimentary facies

CLC Number: 

  • P618.13
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