Lithologic Reservoirs ›› 2017, Vol. 29 ›› Issue (1): 1-10.doi: 10.3969/j.issn.1673-8926.2017.01.001

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Sedimentary facies and controlling factors of coal accumulation of the Upper Permian Xuanwei Formation in Junlian area

ZHANG Tingshan1,2, HE Yingjie1,2, WU Kunyu1,3, LIN Dan4, ZHANG Zhao5   

  1. 1. State Key Laboratory of Oil & Gas Reservoir Geology and Exploitation, Southwest Petroleum University, Chengdu 610500, China;
    2. School of Geoscience and Technology, Southwest Petroleum University, Chengdu 610500, China;
    3. Research Institute of Exploration and Development, PetroChina Qinghai Oilfield Company, Dunhuang 736202, Gansu, China;
    4. Sichuan Key Laboratory of Shale Gas Evaluation and Exploitation, Chengdu 610091, China;
    5. PetroChina Zhejiang Oilfield Company, Hangzhou 310023, China
  • Received:2016-10-25 Revised:2016-12-18 Online:2017-01-21 Published:2017-01-21

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Abstract: The Upper Permian Xuanwei Formation in Junlian area has attracted more attention,which is considered as a potential coalbed methane development zone in the southern margin of the Sichuan Basin. In order to research the distribution and evolution of the coal beds in the Upper Permian Xuanwei Formation,based on the data of drilling,logging and regional geology,combined with the theories and methods of sedimentology and regional geology,this paper divided the sedimentary facies of single well,compared the well- tie section,compiled the map of sedimentary facies,and discussed the controlling factors of coal accumulation. The results show that the Upper Permian Xuanwei Formation mainly developed meandering river facies and tidal flat facies,and a small amount of diamictic platform facies. The coal beds were mainly developed in the swamp microfacies. The warm and humid palaeo-environment prepared good condition for plants blooming. The distribution and development of coal beds in the Upper Permian Xuanwei formation are controlled by tectonic-palaeogeography and palaeoenvironment. This research is significant for understanding coupling relationship of the depositional environment and coal accumulating effect,and favorable for coalbed methane exploration in Junlian area.

CLC Number: 

  • P618.11
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