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《Marine Geology & Quaternary Geology》 2005-02
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THE FORMING CONDITION AND DISTRIBUTION CHARACTERISTICS OF THE GAS HYDRATE IN THE SOUTH CHINA SEA

YAO Bo-chu(Guangzhou Marine Geological Survey, Guangzhou 510075,China)  
We have studied forming condition of gas hydrate in the South China Sea according to the physical oceanography, palaeo-climate, sedimentary environment, and tectonic environment. The researching results tell us that there are different forming conditions of gas hydrate in the South China Sea. In the northeast part of the South China Sea the high salinity water comes from the Philippine Sea, therefore, biologic productivity was high and there was rich organic matter in sediments during the periods of oxygen-isotopes 2,4 and 6. In these periods the sedimentation rate was very high, so there were very good material conditions for formation of gas hydrate. In addition, from the end of Miocene to present, the Philippine Sea plate collided with Asian plate in Taiwan area,extruding the northeast part of the South China Sea along northwest direction. The extruding force made fluid in the sediments very active,and this is very good for the formation of gas hydrate.From the above reason, we believe that there should be rich gas hydrate in the northeast slope of the South China Sea.
【Fund】: 国家重点基础研究发展规划(973)项目(G2000046705);; 国土资源部重大科技项目“中国大陆岩石圈三维结构”
【CateGory Index】: P744.4
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