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《Geoscience》 2009-02
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Gas Hydrate Reservoir Characteristics of Shenhu Area,North Slope of the South China Sea

GONG Yue-hua1,YANG Sheng-xiong1,WANG Hong-bin1,LIANG Jin-qiang1,GUO Yi-qun1,WU Shi-guo2,LIU Guang-hu1 (1.Guangzhou Marine Geological Survey,Guangzhou,Guangdong 510760,China;2.Key Laboratory of Marine Geology and Environment Institute of Oceanology,Chinese Academy of Sciences,Qingdao,Shandong 266071,China)  
As a type of new energy resource,gas hydrate is drawing more and more attention for its cleanness and potential huge energy reserves,whilst the research on hydrate has been developed.However,scientists pay less attention on gas hydrate formation mechanism because relative data are poor.The gas hydrate formation mechanism of Shenhu area,which had been surveyed for nearly four years by Guangzhou Marine Geological Survey,is discussed in this paper in the aspects of substance source,gas transporting conduit,conditions for formation etc.The results suggest that the huge source rocks formed in Paleocene period in Baiyun sag are the main substance source,and diapirs are the main conduit for fluid transportation upwards to form hydrates in the end,while the slip bodies developed broadly in Late Tertiary are the main spaces for gas hydrate accumulation.Finally,The conclusion is drawn that Shenhu area is a better hydrate prospecting area because of its favorable conditions for gas hydrate formation.
【Fund】: 国家重点基础研究发展计划(2009CB219508);; 国土资源部公益性行业科研专项(200811014)
【CateGory Index】: P618.13
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