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《Chinese Journal of Geophysics》 2013-01
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Geothermal history and thermal evolution of the source rocks in the deep-water area of the northern South China Sea

WU Jing-Fu1,YANG Shu-Chun1,ZHANG Gong-Cheng1, SHAN Jing-Nan2,TANG Xiao-Yin2,LIANG Jian-She1 1 CNOOC Research Institute,Beijing 100027,China 2 Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China  
The deep-water area of the northern South China Sea has a significant petroleum potential.Bases on the previous study of the present-day geothermal regime and the reconstructed thermal history from forward modeling,the rift basin model was further constrained by recently obtained vitrinite reflectance and(U-Th)/He data.The results suggest that the thermal history obtained from the basin model is suitable to calculate the maturation of the source rocks and there are four hydrocarbon generation centers in the deep-water area,namely,the Baiyun sag in Pearl River Mouth Basin,Ledong sag,Lingshui Sag and Songnan sag in Qiongdongnan Basin.In the hydrocarbon generation centers,the source rocks are of over-maturation and the gas is the major hydrocarbon production.Because of the effect of the heat flow from the basin basement,the source rocks maturated rapidly from 32 Ma to 23.3 Ma in the whole study area.The other rapid maturation processes occurred in present-day(after 2.48 Ma) in Qiongdongnan Basin but not in Pearl River Mouth Basin.
【Fund】: 国家科技重大专项大型油气田及煤层气开发专项“海洋深水油气勘探关键技术”(2008ZX050002025)资助
【CateGory Index】: P618.13
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