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Article Navigation >  Acta Sedimentologica Sinica  > 2002  >  20(1): 156-159

GAO Gang, HUANG Zhi-long. Research on Organic Inclusion in Reservoir and Gas Accumulation Process in Pingluoba Gas Field[J]. Acta Sedimentologica Sinica, 2002, 20(1): 156-159.
Citation: GAO Gang, HUANG Zhi-long. Research on Organic Inclusion in Reservoir and Gas Accumulation Process in Pingluoba Gas Field[J]. Acta Sedimentologica Sinica, 2002, 20(1): 156-159.
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Research on Organic Inclusion in Reservoir and Gas Accumulation Process in Pingluoba Gas Field

  • University of Petroleum, Beijing 102200

  • Received Date: 2000-12-30
  • In this paper, the author researched diagenesis and organic inclusion in reservoir. In this area, organic inclusions were mostly formed by recrystalization and metaspmasis and with various phases. They distributed chiefly in dissolved seams and pores in quartz grains and not in structure slot. The organic inclusion abundance in Upper Triassic was more than that in Shaximiao Formation. The homogenization temperature of organic inclusion was between 100℃ and 110℃ in the second interval of Xujiahe Formation and between 90℃ and 100℃ in Shaximiao Formation. The second segment gas reservoir of Xujiahe Formation was formed earlier and underwent the course early from small charge to large charge and late again from adjustment to small charge. The gas reservoir of Shaximiao Formation was formed in the course of Xishan Tectonic Movement.
  • [1] 曹伟,安凤山,王允诚等.致密砂岩天然气藏地质特征[J].矿物学报,1998,73(18):39～44
    [2] 周江羽,吴冲龙,韩志军等.川西坳陷天然气成藏条件与成藏模式[J].四川地质学报,1998,18(2):116～120
    [3] 李少虎,吴冲龙,王华等.四川盆地香家河组地层格架与天然气藏成藏的关系[J].石油与天然气地质,1998,19(2):146～151
    [4] 刘斌,贝东,王菁.四川西北部陆相地层异常高压的形成与演化[J].天然气工业,1995,19(3):8～11
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  • Received:  2000-12-30

Research on Organic Inclusion in Reservoir and Gas Accumulation Process in Pingluoba Gas Field

  • University of Petroleum, Beijing 102200
  • Received Date: 2000-12-30

Abstract: In this paper, the author researched diagenesis and organic inclusion in reservoir. In this area, organic inclusions were mostly formed by recrystalization and metaspmasis and with various phases. They distributed chiefly in dissolved seams and pores in quartz grains and not in structure slot. The organic inclusion abundance in Upper Triassic was more than that in Shaximiao Formation. The homogenization temperature of organic inclusion was between 100℃ and 110℃ in the second interval of Xujiahe Formation and between 90℃ and 100℃ in Shaximiao Formation. The second segment gas reservoir of Xujiahe Formation was formed earlier and underwent the course early from small charge to large charge and late again from adjustment to small charge. The gas reservoir of Shaximiao Formation was formed in the course of Xishan Tectonic Movement.

GAO Gang, HUANG Zhi-long. Research on Organic Inclusion in Reservoir and Gas Accumulation Process in Pingluoba Gas Field[J]. Acta Sedimentologica Sinica, 2002, 20(1): 156-159.
Citation: GAO Gang, HUANG Zhi-long. Research on Organic Inclusion in Reservoir and Gas Accumulation Process in Pingluoba Gas Field[J]. Acta Sedimentologica Sinica, 2002, 20(1): 156-159.
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