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《Acta Sedimentologica Sinica》 2002-02
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The Origin of Natural Gases and Geochemistry Characters ofChangxing Reef and Feixianguan Oolitic Beach Gas Reservoirs in Eastern Sichuan Basin

YANG Jia-jing~1 WANG Yi-gang~1 WANG Lan-sheng~1 WEN Ying-chu~1 LIU Hua-yi~1 Zhou Guo-yuan~2 1(Institute of Exploration and Development, Southwest Oil and Gas Field Branch Company, PetroChina, Subkey Laboratory of Carbonate Gas Reservoir Formatio  
Changxing Reef of Upper Permian and Feixianguan oolitic beach of Lower Triassic are the focus point of exploration work in Sichuan Basin during the ninth-five-year-plan. Through the study on organic geochemistry of source rocks of Upper Permian and Lower Triassic, reservoir bitumen and natural gases of Changxin Fm. reef and Feixianguan Fm. oolitic beach gas reservoirs, the shoreside coal measures mudstone and the sea trough carbonate of Upper Permian Series have been defined as the main source rocks,which are high maturate and controlled by the different sedimentary facies, and the reservoir bitumen and natural gases of Changxing Fm. reef and Feixianguan Fm. oolitic beach gas reservoirs are originated from the source rock of Upper Permian Series, the natural gas is a dry gas being thermally degraded from oil, the solid bitumen is a residue of oil retained in reservoir rocks, and the migration of natural gases is mainly vertical. The volume of H 2S is high in some exploratory wells of Feixianguan Fm. oolitic beach gas reservoirs, such as Gaofengchang, Longmen, Tieshanpo, Dukouhe, Luojiazhai structure, etc. H 2S is associated with the distribution of anhydrite in Feixianguan Fm. oolitic beach reservoir and related with the thermochemical sulfate reduction (TSR).And all above are closely related with the sedimentary facies.
【Fund】: “九五”国家重点科技攻关项目“四川盆地东北部长兴组—飞仙关组气藏形成条件研究”(编号 :99 1 1 0 0 2 0 1 0 4 )部分成果。
【CateGory Index】: P593;P618.13
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