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《Chinese Journal of Geophysics》 2009-07
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Genetic model of the hydrate system in the fine grain sediments in the northern continental slope of South China Sea

WU Shi-Guo~1,DONG Dong-Dong~1,YANG Sheng-Xiong~2,ZHANG Guang-Xue~2,WANG Zhi-Jun~3,LI Qing-Ping~3,LIANG Jin-Qiang~2,GONG Yue-Hua~2,SUN Yun-Bao~(1,4)1 Key Laboratory of Marine Geology and Environment,CAS,Qingdao 266071,China2 Guangzhou Marine Geological Survey,Guangzhou 510075,China3 Beijing Research Center,CNOOC,Beijing 100027,China4 Graduate University of the Chinese Academy of Sciences,Beijing 100049,China  
Gas hydrate samples were obtained firstly in China by drilling on the northern margin of South China Sea (SCS).To understand the formation mechanism of this unique accumulation system,this paper discusses the factors controlling the formation of the system by accurate geophysical interpretation and geological analysis,based on the high precision 2-D and 3 D multichannel seismic data in the drilling area.There are three key factors controlling the accumulation of the gas hydrate system in fine grain sediment:(1) large volume of fluid bearing methane gas joins the formation of gas hydrate.Active fluid flow in the northern South China Sea makes both thermal gas and/or biogenic gas migrate into shallow strata and form hydrate in the gas hydrate stability zone (GHSZ).The fluid flow includes mud diapir and gas chimney structure.They are commonly characterized by positive topographic relief,acoustic turbidity and push-down,and low reflection intensity on seismic profiles.The gas chimneys can reach to GHSZ,which favors the development of BSRs.It means that the active fluid flow has a close relationship with the formation and accumulation of gas hydrate.(2) The episodic process of fracture plays an important role in the generation of gas hydrate.It may provide the passage along which thermogenic or biogenic gas migrated into gas hydrate stability zone (GHSZ) upward.And it increases the pore space for the growth of hydrate crystal.(3) Submarine landslide induced the anomalous overpressure activity and development of fracture in the GHSZ.The formation model of high concentration gas hydrate in the drilling sea area was proposed on the basis of above analysis.
【Fund】: 中国科学院重要方向性项目“南海深水油气勘探中若干问题(KZCX2-YW-203)”;; “国家863高技术项目(2006AA09Z349)”资助.
【CateGory Index】: P744.4
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