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Fluid Inclusion Study and Its Application to Tracing Gas-Trapping History in the Qingshen Gas Field of the Songliao Basin

JI Xue-yan1, SHU Ping1, QU Yan-ming1, DING Ri-xin1, GUO Zhen-hua2, WANG Pu-jun2   

  1. 1.Daqing Exploration &Development Institute, Daqing, Heilongjiang 163712, China;2.College of Earth Sciences, Jilin University, Changchun 130061, China
  • Received:2006-10-10 Revised:1900-01-01 Online:2007-07-26 Published:2007-07-26
  • Contact: WANG Pu-jun

Abstract: Microscopic inspection, microthermometry and salinity measurement, systematic fluid inclusion studies in the Qingshen gas field of the Songliao Basin show that homogenization temperature of fluid inclusion varies from 97.1℃ to 156.7℃ in the reservoir. Through comprehensive analysis, we found that there are 6 thermal fluid activities and 4 charging periods of gas in the volcanic reservoir of the Yingcheng Formation in Xujiaweizi rift. Average homogenization temperature ranges recorded by hydrocarbon-bearing salt-water inclusions are 97.1℃ to 114.1℃, 121.4℃ to 128.3℃, 130.5℃ to 138.2℃ and 140.6℃ to 156.7℃, respectively. Regional burial history and other factors being considered, the third thermal fluid activity, which spans the time range from late Quantou Formation to middlelate Qingshankou Formation, is considered as a major period in which massive natural gas pools was formed among all periods charging of gas in the Yingcheng Formation reservoir in Xujiaweizi rift.

Key words: Qingshen gas field of the Songliao Basin, volcanic gas pool, fluid inclusion, homogenization temperature, hydrocarbon gas infilling

CLC Number: 

  • P618.13
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