{"refrec":{"BRefID":240752,"RR":"<b>Wang, H.; Yuan, S.; Gao, H.</b> (2010). The contourite system and the framework of contour current circulation in the South China Sea. <i>Geo-Temas 11</i>: 189-190","BEntID":232449,"PublicFlag":1,"CheckedFlag":0,"wosflag":null,"vabbflag":null,"RefStringPartII":". <i>Geo-Temas 11</i>: 189-190","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Wang, H.; Yuan, S.; Gao, H.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Wang, H. <i>et al.</i>","Englishabstract":"Based on the data-base including single and multi-channel seismic data, piston core, seafloor photograph of the northern margin of the South China Sea, the depositional facies constituting by gravity-flow, contourite current and hybrid depostional system is constructed. The source of contour-current is traced from the western Philippine deep-water mass, the watermass intrude the South China Sea through the Luzon Strait, encircling the northern margin to the western margin and eventually dissipate in the biggest upwelling zone of the South China Sea, and enter the surface current circulation. 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