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《Geoscience》 2008-03
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Marine Gas Hydrate System:State of the Art

WU Neng-you1,2,LIANG Jin-qiang2,WANG Hong-bin2,SU Xin3,SONG Hai-bin4,JIANG Shao-yong5,ZHU You-hai6,LU Zhen-quan6(1.Key Laboratory of Renewable Energy and Gas Hydrate,Guangzhou Institute of Energy Conversion,Chinese Academy of Sciences,Guangzhou,Guangdong 510640,China;2.Guangzhou Marine Geological Survey,Guangzhou,Guangdong 510075,China;3.School of Marine Geosciences,China University of Geosciences,Beijing 100083,China;4.Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China;5.State Key Laboratory for Mineral Deposits Research,Nanjing University,Nanjing,Jiangsu 210093,China;6.Institute of Mineral Resources,Chinese Academy of Geological Sciences,Beijing 100037,China)  
Based on the summary of research progress on gas sources and formation mechanisms,geophysical and geochemical proxies,formation environments and geological models,distribution of marine gas hydrate,this paper points out and discusses the direction and scientific issues for formation mechanism research of marine gas hydrate in China.Many scientific data and samples such as the wire-line logging,in-situ temperature,properties,geochemical data and sediment cores,pore water,head space and void gas,microbiology samples,etc,were obtained through the gas hydrate drilling expedition in Shenhu area of the north slope of South China Sea in April-June 2007.So,Shenhu area is an ideal area for the research on formation mechanism and distribution pattern of marine gas hydrate.Focusing on the material basis,formation environment and process,responding index and formation system of gas hydrate,a series of research in the light of the interaction between gas,water,sediment and gas hydrate,geophysical and geochemical responding mechanism,coupling control of different conditions for gas hydrate formation should be carried out on the north slope of South China Sea.
【Fund】: 中国科学院百人计划项目;; 国土资源部公益性行业科研专项经费项目(2008334014)
【CateGory Index】: P744.4
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