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《Journal of Guilin University of Technology》 2009-03
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Geochemistry of Saline Lacustrine Facies Oil From Member 3 of Shahejie Formation in Dongpu Depression of Wenliu

ZHANG Qing-feng1,2,SHEN Zhong-min1,2,PAN Zhong-liang1,2,Luo Xiao-ping 1,2,CHANG Zhen-heng3,YANG Xi4(1.State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation,Chengdu University of Technology,Chengdu 610059,China;2.College of Energy Resources,Chengdu University of Technology,Chengdu 610059,China;3.Research Institute of Exploration and Development,Zhongyuan Oilfield Company,PetroChina,Puyang 457001,China;4.Department of Exploitation,Tarim Oilfield Company,PetroChina,Kuerle 841000,China)  
Group composition and carbon isotope of oil,chromatogram and mass spectrum of aliphatic are analyzed from samples source rock,crude oil and oil sand in Wenliu area Dongpu depression.The group composition of crude oil shows high contents of saturated hydrocarbons,aromatics and low non-hydrocarbon and asphaltene.The characteristics of carbon isotope similar to that of marine organic matter,indicate that organic matter mainly originated from the Salt Lake farcies aquatic organisms and bacteria.There is predominance of phytane to pristane:the range of parameter of C29αα 20S/(20S+20R) is 0.37~0.57,and C29ββ/(ββ+αα) is 0.41~0.65 respectively.The contents of Diastenranes and γ-acerance are relatively high,the index of γ-acerance reaches 0.55~0.84.Geochemistry of oil above shows that crude oil formed in a typical salt lake facies and oxygen-free environment.The results of comparative analysis of oil and the source rock show that crude oil from Member 3 of Shahejie Formation in Wenliu is closely related to source rocks of Member 3 of Shahejie Formation,and its source rock is the mudstone of Member 3 of Shahejie Formation.
【Fund】: 中石化科技攻关项目(P04022)部分研究成果
【CateGory Index】: P618.13
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