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2015, 34(4) 1052-1060 DOI:
ISSN: 1004-5589 CN: 22-1111/P |
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Gas accumulation in lithologic reservoirs of deep half- graben rift in Songliao Basin: a case of Wangfu Fault Depression |
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DAI Deng-Liang, DONG Qing-Shui, REN Yan-Ning, WANG Ji-Yuan, LIU Zhe, ZHANG Hang |
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1. College of Earth Sciences��Jilin University��Changchun 130061��China; 2. Key Laboratory for Oil Shale and Coexistent Energy Minerals of Jilin Province of Jilin University��Changchun 130061��China |
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Abstract��
Seismic��drilling and testing data analyses indicate that the gas reservoir types of Wangfu Fault Depression mainly include the volcanic dome- lithological type��sandstone on the tip off type and lens type�� The volcanic dome inside which has reservoir section together with the source- rock of Huoshiling or Shahezi Formation constituted beneficial source- reservoir- seal assemblage��which is the basis of volcanic dome structural- lithologic gas reservoir�� The finger- like interaction between fan delta updip pinchout lobate sand body of synsedimentary fault boundary and high- quality source rock is essential to the formation of updip pinchout lithologic gas reservoirs�� The source- rock of Shahezi Formation which enveloped the collapsed gravity flow of loose volcanic cone in Huoshiling Formation is the key factor of forming lens- shaped lithologic gas reservoirs�� Furthermore��this paper summarized the gas accumulation mode of Wangfu Fault Depression��and points out that the faulted slope area is the favorable accumulation region of updip pinchout lithologic reservoirs��and the secondary uplift area is superimposed accumu- lation zones of volcanic dome structure- lithologic gas reservoirs of Huoshiling Formation and lens lithologic gas res- ervoirs of Shahezi Formation�� It is the adjacent raised edge zone of the secondary depression groove that tends to form volcanic dome gas reservoirs�� |
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Keywords��
Songliao Basin
Wangfu Fault Depression
lithologic gas reservoir
reservoir controlling fac- tors
law of reservoir formation
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