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作 者:Shuangjian Li Wei Sun Yingqiang Li Jian Gao Zhiyuan Liu Xiaokuan Feng
机构地区:[1]Key Laboratory of Geology and Resources in Deep Stratum,SINOPEC,Beijing,102206,China [2]SINOPEC Petroleum Exploration&Production Research Institute,Beijing,102206,China [3]School of Energy Resources,China University of Geosciences,Beijing,100083,China
出 处:《Energy Geoscience》2023年第3期80-89,共10页能源地球科学(英文)
基 金:the National Natural Science Foundation of China(No.U19B6003;U20B6001);the Chinese Academy of Sciences(No.XDA14000000).
摘 要:No breakthrough has been made in petroleum exploration of the Sinian Dengying Formation in the southeastern Sichuan Basin as the major factors controlling the hydrocarbon accumulation of the Dengying Formation have not been well established,including the development period and distribution of the platform margin,the effectiveness of the source-reservoir combination and the reliability of the Cambrian pre-salt structural trap.Based on the interpretation of seismic data and hydrocarbon-source correlation,the distribution of the platform margin of the Sinian Dengying Formation in the southeastern Sichuan Basin was mapped.Moreover,the gas source rocks of the Dengying Formation were clarified according to geochemical characteristics of fluid inclusions,and the pre-salt structures were further confirmed by seismic forward modeling and experiments of prestack depth migration.Results showed that the sedimentary facies of the 4th member of Dengying Formation in the southeastern Sichuan Basin was platform margin of gentle slope type.The platform margin reservoir of the Dengying Formation and the Lower Cambrian source rocks constitute a favorable source-reservoir combination.The carbon isotope characteristics of gas in fluid inclusions indicate that some of the oil/gas in the Dengying Formation were contributed by the Doushantuo Formation source rocks.As the difference in seismic velocities between carbonate rocks and gypsum/salt beds may cause a reduction in the amplitude of pre-salt structures,the low-amplitude structures identified on current seismic profiles are underestimated instead of overestimated.Accordingly,the Sinian structural traps are confirmed to develop in the deep pre-salt sequences in the low-steep anticline belt,southeastern Sichuan Basin.On the basis of the above new understanding,we propose two types of hydrocarbon migration modes for the Sinian Dengying Formation in southeastern Sichuan Basin,including lateral migration of hydrocarbons generated from the Cambrian Qiongzusi Formation and vertical migrat
关 键 词:Source-reservoir combination Fluid inclusion Play fairway Dengying formation Southeastern Sichuan Basin
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