Lithologic Reservoirs ›› 2024, Vol. 36 ›› Issue (6): 169-180.doi: 10.12108/yxyqc.20240616

• PETROLEUM EXPLORATION • Previous Articles     Next Articles

Characteristics and genetic mechanism of condensate oil and gas of the Jurassic Sangonghe Formation in western well Pen-1 sag，Junggar Basin

QIAO Tong1,2, LIU Chenglin1,2, YANG Haibo3, WANG Yifeng4,5, LI Jian4,5, TIAN Jixian4,5, HAN Yang3, ZHANG Jingkun1,2   

  1. 1. State Key Laboratory of Petroleum Resources and Engineering, China University of Petroleum(Beijing), Beijing 102249, China;
    2. College of Geosciences, China University of Petroleum(Beijing), Beijing 102249, China;
    3. Research Institute of Exploration and Development, PetroChina Xinjiang Oilfield Company, Karamay 834000, Xinjiang, China;
    4. PetroChina Research Institute of Petroleum Exploration & Development, Beijing 100083, China;
    5. Key Laboratory of Gas Reservoir Formation and Development, CNPC, Langfang 065007, Hebei, China
  • Received:2023-10-25 Revised:2023-12-26 Online:2024-11-01 Published:2024-11-04

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Abstract: Based on the analysis and test data of petroleum geochemistry，oil test and phase behavior analysis of condensate gas，basin modeling techniques were used to determine the characteristics，accumulation process and genetic mechanism of condensate gas reservoirs of Jurassic Sangonghe Formation in Qianshao well area of western well Pen-1 sag，Junggar Basin. The results show that：（1）The condensate reservoirs of Jurassic Sangonghe Formation are structural-lithologic reservoirs in western well Pen-1 sag. The high-quality reservoirs are mainly composed of gray fine-medium feldspathic detritus sandstone，with porosity ranging from 2.70% to 16.1%，an average value of 12.10%，permeability ranging from 0.016 mD to 109.000 mD，an average value of 14.17 mD. The reservoirs belong to middle porosity and low permeability reservoirs，and form reservoir-cap assemblage with two sets of source rocks from the underlying Permian Fengcheng Formation and lower Urho Formation.（2）The condensate oil in the study area is the product of the source rocks of lower Urho Formation within mature to high-mature stage，it has physical properties of low density，low viscosity，low freezing point and low wax content，and its n-alkanes are composed of low and medium carbon components.（3）The natural gas of condensate gas reservoirs in the study area is mainly composed of hydrocarbon gas，with concentrated distribution of methane and ethane carbon isotope values ranging from -37.40‰ to -36.84‰ and -27.55‰ to -26.54‰，respectively. It was derived from the cracking of humic-type source rocks of lower Urho Formation. （4）The condensate oil and gas generated by the source rocks of lower Urho Formation in the early Paleogene were continuously adjusted and finally charged in the early Neogene to form the present condensate gas reservoirs. The fluid composition has not changed since the reservoir formation，and the fluid phase type is also unchanged，so it is a primary condensate gas reservoir.

Key words: condensate oil, condensate gas reservoir, humic-type cracking gas, source rocks of lower Urho Formation, phase type of reservoir, Sangonghe Formation, Jurassic, western well Pen-1 sag, Junggar Basin

CLC Number: 

  • TE122.1
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