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《Petroleum Exploration and Development》 2010-03
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Hot fluid activities and the hydrocarbon accumulation in the PY30-1 structure of Panyu Low Uplift,Pearl River Mouth Basin

Guo Xiaowen1,He Sheng1,Shi Hesheng2,Zhu Junzhang2(1.Key Laboratory of Tectonics and Petroleum Resources,China University of Geosciences,Wuhan 430074,China;2.Institute of CNOOC Ltd.Shenzhen,Guangzhou 510240,China)  
PY30-1 structure,accompanied with the development of diapirs,is an important petroliferous structure.To clarify the process of hydrocarbon accumulation,hot fluid activities were confirmed in the PY30-1 structure of the Panyu Low Uplift,the origin of oil and gas and the evolution of overpressure were studied and the hydrocarbon accumulation was analyzed.Hot fluid activities occurred in the PY30-1 structure,as evidenced by vitrinite reflectance(Ro),smectite-illite mineral abnormal transformation,and fluid inclusion homogenization temperatures.Migration of hydrocarbons happened with the hot fluids activities.The source rocks of the oil and gas in the PY30-1 structure are dominantly the Enping Formation lacustrine mudstones,secondarily the Wenchang Formation mudstones.The formation pressure evolution modeling reflects that there are 3 stages of overpressure release at 37-40 Ma,31-33 Ma and 0-16 Ma under the influence of the second phase of the Zhuqiong movement,the Nanhai movement,and the Dongsha movement.The third stage of overpressure release is coincident with the hydrocarbon charging times.The hydrocarbon accumulation in the PY30-1 structure is that that the hydrocarbon expulses from the source rocks because of overpressure release in the Baiyun Depression under the influence of the Dongsha movement and then migrates vertically through the faults in diapirs.
【Fund】: 国家重点自然科学基金项目(40238060);; 中国地质大学构造与油气资源教育部重点实验室开放基金项目(TPR-2009-07)
【CateGory Index】: P618.13
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