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《Journal of Chengdu University of Technology(Science & Technology Edition)》 2006-03
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An analysis of the structural background of the sedimentation of the Zhujiang deep-water fan system in the South China Sea

WU Chang-rong~1,PENG Da-jun~1,PANG Xiong~2,YE Bin~1,SHU Yu~21.College of Energy Resources,Chengdu University of Technology,Chengdu 610059,China;2.Shenzhen Branch of China National Offshore Oil Company Ltd.,Guangzhou 510240, China  
The turbidite system in the intraslope basin of continental margin is one of the biggest hot spots of deep-water oil and gas exploration and development in recent years.A typical deep-water fan system has been discovered in Pearl River Mouth Basin of the north continental margin of South China Sea.It is the Zhujiang deep-water fan system in South China Sea.It has a giant oil and gas potential.Whether has it the structural background of sedimentation of intraslope basin? An integrated analysis is carried out to the structural background characteristic of sedimentation of the Zhujiang deep-water fan system in South China Sea from the point of view of deep-water fan system,mainly based on the integrated interpretation of 700 km long cables and deep reflection(14 s) seismic data acquired recently(the cable passes through the entire Baiyun sag),and combined with the research results of Ocean Drilling Program in South China Sea(ODP1148 sit).The research shows some results as follows.The Baiyun sag is an intraslope basin on the north continental margin in South China Sea from early Miocene to middle Miocene(i.e.about 25 Ma B.c.~ 10 Ma B.c.).It formed by continuous subsidence of the basin base in the period of depression and the associated tectonic activities.The intraslope basin in Baiyun sag is different from some others on many passive continental margins in the world(for example,West Africa offshore,Brazil offshore,the Gulf of Mexico).Some geological forces,e.g.eustatic change,change of sediment flux,tectonic activity and so on,have important effects on the Zhujiang deep-water fan system in South China Sea in different periods in some degree on the structural background of intraslope basin.In brief,it is the intraslope basin that has favored the formation of the Zhujiang deepwater fan system in South China Sea.This is of great significance for a further comprehensive study on the mechanism of formation,the evolutionary process,the structure characteristic and some others of the Zhujiang deep-water fan system in South China Sea henceforth.
【Fund】: 国家自然科学基金重点资助项目(40238060)
【CateGory Index】: P736.21
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9 CHAI Yucheng1, ZHOU Zuyi2(1.Department of Earth Sciences , National Natural Science Foundation of China,Beijing 100085,China; 2.Laboratory of Marine Geology,Tongji University, Shanghai 200292,China);SCIENTIFIC OCEAN DRILLING:ACHIEVEMENTS AND PROSPECTS[J];Advance in Earth Sciences;2003-05
10 ZHONG Guangfa(Laboratory of Marine Geology, Tongji University, Shanghai 200092, China);CAUSES AND EFFECTS OF SEA-LEVEL CHANGE[J];Advance in Earth Sciences;2003-05
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