2011
DOI: 10.1016/j.margeo.2011.05.010
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Influence of the Kuroshio current intrusion on depositional environment in the Northern South China Sea: Evidence from surface sediment records

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Cited by 65 publications
(39 citation statements)
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“…8), surprisingly little research has focused on details of the transport mechanisms of the heavy minerals in these deposits. Previous studies on sediment transport on the northern shelf of the SCS have been based on clay mineral analyses and bulk-rock geochemistry, which have demonstrated the presence of surface and deep-water currents, including the Guangdong Longshore Current (GDLC), the SCS Warm Current (SCSWC), the SCS Branch of the Kuroshio Current (SCSBK), and the Branch of the North Pacific Deep Water Current (BNPDWC), which are the most important currents transporting sediments to the northern SCS from various provenances (Cai et al, 2013;Liu et al, 2011Liu et al, , 2012Liu et al, , 2013Liu Z.F. et al, 2008Liu Z.F.…”
Section: Transport Mechanismsmentioning
confidence: 99%
“…8), surprisingly little research has focused on details of the transport mechanisms of the heavy minerals in these deposits. Previous studies on sediment transport on the northern shelf of the SCS have been based on clay mineral analyses and bulk-rock geochemistry, which have demonstrated the presence of surface and deep-water currents, including the Guangdong Longshore Current (GDLC), the SCS Warm Current (SCSWC), the SCS Branch of the Kuroshio Current (SCSBK), and the Branch of the North Pacific Deep Water Current (BNPDWC), which are the most important currents transporting sediments to the northern SCS from various provenances (Cai et al, 2013;Liu et al, 2011Liu et al, , 2012Liu et al, , 2013Liu Z.F. et al, 2008Liu Z.F.…”
Section: Transport Mechanismsmentioning
confidence: 99%
“…The northern SCS is an area of active sedimentation with possible input of terrigenous sediment from the Pearl, Red and Yangtze rivers, as well as the islands of Taiwan and Luzon (Shao et al, 2009;Wan et al, 2007). After these river-derived terrigenous sediments enter the sea, most are deposited on the continental shelf, but a small amount is transported further where it is deposited on the abyssal basin (Liu et al, 2011). Regardless, sediment transport and depositional dynamics involve ocean circulation, which is comparatively complex in the SCS (Wan et al, 2010).…”
Section: Introductionmentioning
confidence: 99%
“…Monsoon winds after (Webster 1994); surface current after (Shaw and Chao 1994;Fang et al 1998;Hu et al 2000); deep current deduced from (Qu et al 2006); longshore current after (Wang et al 1986). Numbers for winter and summer currents (Fang et al 1998;Li et al 1998;Hu et al 2000;Caruso et al 2006;Liu et al 2010Liu et al , 2011Liu et al , 2012: 1, Guangdong Coastal Current; 2, SCS Warm Current (SCSWC); 3, NW Luzon Coastal Current; 4, NW Luzon Cyclonic Eddy; 5, NW Luzon Cyclonic Gyre; 6, SCS Branch of Kuroshio (SCSBK); 7, Loop Current; 8, Longshore Current; 9, Deep water Current.…”
Section: Current Systems Effects On Sea-surface Chl-a Concentrationmentioning
confidence: 99%
“…Compared with large amounts of sediments from the Pearl River and Taiwan Island, sediment discharge from Luzon Island is limited (Liu et al 2011). Sediments from Luzon Island are confined within the northwest of Luzon Island and hardly transported to the northern shelf of the SCS throughout the SCSBK flow route.…”
Section: Current Systems Effects On Sea-surface Chl-a Concentrationmentioning
confidence: 99%