Journal of Jilin University(Earth Science Edition) ›› 2019, Vol. 49 ›› Issue (3): 650-661.doi: 10.13278/j.cnki.jjuese.20180071

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Sedimentary Characteristics and Genesis of Middle Jurassic Conglomerates of Haifanggou Formation in Beipiao Basin, Western Liaoning

Zhao Jiaqi1, Gao Youfeng2,3, Liu Haibo1, Wang Qingbin4, Zhang Yan1, Wang Pujun1,2   

  1. 1. College of Earth Sciences, Jilin University, Changchun 130061, China;
    2. Key Laboratory for Evolution of Life and Environment in Northeast Asia(Jilin University), Ministry of Education, Changchun 130026, China;
    3. Research Center of Paleontology and Stratigraphy, Jilin University, Changchun 130026, China;
    4. Tianjin Branch of CNOOC China Ltd., Tianjin 300459, China
  • Received:2018-04-04 Online:2019-06-03 Published:2019-06-03
  • Supported by:
    Supported by Technological Project of Tianjin Company, CNOOC(CCL2018TJXSWST0084) and National Key R & D Program of China(2017YFC0601405)

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Abstract: The sedimentary characteristics and genesis of the Middle Jurassic conglomerates in Haifanggou Formation were determined by measuring the 2 705 m long two sections,identifying 40 micro-sections,and analyzing 419 gravel statistical particle size in Beipiao basin in western Liaoning. The main lithology of Haifanggou Formation in the northwest Liaoning is a set of compound conglomerate which is an alluvial fan facies including two series of intermediate-acid volcanic rocks,namely the lower effusive facies,air-fall and pyro-clastic flow deposit of explosive facies. The source of Haifanggou Formation is from the SSW area,where the Archaean metamorphic rock, crystalline basement and the volcanic rocks of Xinglonggou Formation in the Lower Jurassic were generally rapidly uplift and denuded. Based on the study of the tectonic setting of the area, the boundary between Beipiao Formation and Haifanggou Formation and the sedimentary characteristics of Haifanggou Formation, the multicomponent conglomerate is an important product of the tectonic movement of compression and extension in the second phase of Yanshanian movement, and the two series of intermediate-acid volcanic rocks are the important indicators of volcanic eruption.

Key words: Haifanggou Formation, lithofacies, gravel statistics, sedimentary characteristics, provenance, paleo-current, Yanshanian movement, Beipiao basin

CLC Number: 

  • P588.212
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