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《Marine Geology & Quaternary Geology》 2002-01
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SEISMIC RECOGNITION STUDIES ON MARINE GAS HYDRATE

MA Zai-tian 1, GENG Jian-hua 1, DONG Liang-guo 1, SONG Hai-bin 2 ( 1Laboratory of Marine Geology, Tongji University, Shanghai 200092, China; 2Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China)  
Gas hydrate is to support the survival and development of human beings as a new natural energy for the 21st century. It was proven in 1960's, that Messoyakha, a large gas field in Siberia of Russia was a typical field composed of natural gas hydrate, and in 1970's, solid gas hydrate samples were collected from seafloor. In 1971, R Stoll for the first time interpreted BSR (bottom simulating reflector) in seismic sections as the marker of the existence of marine gas hydrate, and the interpretation was confirmed by the following deep-sea drillings. And from then on, this seismic method has become important means to study natural gas hydrate in wide area. Recognition methods of gas hydrate are represented by BSR recognition technique, seismic parameter inversion study, seismic digital modeling and physical modeling, reserves estimation and data hi-fi processing. These methods are interdependent and controlling on each other and can be taken as integration. If we pay much attention to individual method and neglect the comprehensive study done by the integration, the effectiveness of the seismic recognition will be limited. According to some preliminary results got from researching processes, sea areas favorable for the formation of gas hydrate in China are the Okinawa Trough in the East China Sea, area off eastern coast of Taiwan, continental margin in the north of the South China Sea and the Nansha Trough. The present studies, however, are just at the beginning and needed to be proven. Much work should be done to innovate on traditional behaviors and not to exactly follow foreign models and China's own specialties should be considered.
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【CateGory Index】: P744;P631.4
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