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《Journal of Marine Sciences》 2006-04
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A study on the seismic reflection of the gas hydrate distribution at the northeast SCS slope and Hengchun ridge

SHANG Ji-hong,LI Jia-biao(Second Institute of Oceanography,SOA,Laboratory of Submarine Geosciences,SOA,Hangzhou 310012,China)  
By analyzing and interpreting the newly acquired seismic profile supported by national 973 investigation projects and synthesizing the data with the other related geologic and geographic information,we support the argument that the reflections located at the northeast SCS slope and Hengchun ridge are the Bottom Simulated Reflection(BSR) as shown on the seismic profile.The genesis of the gas hydrate in these two areas is different because of the different regional tectonics and geologic environment.The gas hydrate located at the northeast SCS slope is related to the broadly existed fracture zone,slumping accretion and the distinctive environment of pressure masking field caused by them.But the genesis of the gas hydrate at the Hengchun ridge is associated with the thrust nappe structured accretionary wedges formed along Manila subduction zone and the related sea-floor fluid channel system constructed by them and other faults.Since the analogous geologic bodies are broadly distributed at the SCS and the temperature-pressure environment is very suitable for the formation and deposition of the gas hydrate,we suggest that much more of this resource should be stored in this area.
【Fund】: 国家重点基础研究发展规划资助项目(G2000046700)
【CateGory Index】: P744.4
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