Features of gas geology and its main controlling factors in Pingxiang mining area, Jiangxi Province

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• 作者：Zhi-gen Zhao (1) (2)
  Jia-ping Yan (3)
  Xing Liu (3)
  
• 关键词：Pingxiang Mining Area ; coal and gas outburst ; gliding nappe ; coal rank ; surrounding rock
• 刊名：Journal of Coal Science and Engineering (China)
• 出版年：2012
• 出版时间：September 2012
• 年：2012
• 卷：18
• 期：3
• 页码：271-275
• 全文大小：461KB
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• 作者单位：Zhi-gen Zhao (1) (2)
  Jia-ping Yan (3)
  Xing Liu (3)
  
  1. School of Earth and Environment, Anhui University of Science and Technology, Huainan, 232001, China
  2. Mine Geology Committee, China Coal Society, Huainan, 232001, China
  3. School of Surveying, Anhui University of Science and Technology, Huainan, 232001, China
  
• ISSN：1866-6566

文摘

Pingxiang Mining Area in Jiangxi Province is one of the major coal-producing areas and is prone to serious coal and gas outburst, therefore, it is of significance to research on gas geological features and its controlling factors. Based on the analysis of gas data collected from geological exploration and coal mining, the research reveals that the features of gas geology vary significantly between west part and east part of Pingxiang Mining Area, and it is characterized by high gas mines with serious coal and gas outburst in the west part and low gas mines with no coal and gas outburst in the east part. The main controlling factors to gas geology are discussed, and the great difference of gas geology between west part and east part is the result of comprehensive effect by geological factors. Concerning the gas generation, the coal rank in the west part is higher than that in the east part, which is favorable to generate more gas in the west part than in the east part. Concerning the gas preservation, the structures are characterized by gliding nappe in the west part and by tectonic window in the east part, the surrounding rocks are characterized by poor permeability in the west part and comparatively good permeability in the east part, and the characteristics of coal rank and coal body structure are favorable to gas preservation in the west part and favorable to gas emission in the east part.