Scheuer C;Gohl K;Udintsev G,Bottom-current control on sedimentation in the western Bellingshausen Sea,West Antarctica,Geo-Marine Letters,2006.
[6]
Sejrup H P;Haflidason H;Hjelstuen B O;Nyg(a)rd A Bryn P Lien R,Pleistocene development of the SE Nordic Seas margin,Marine Geology,2004.
[7]
Shanmugam G;Spalding T D;Rofheart D H,Process sedimentology and reservoir quality of deep-marine bottom-current reworked sands(sandy contourites):an example from the Gulf of Mexico,AAPG Bulletin,1993.
[8]
Shanmugam G;Spalding T D;Rofheart D H,Traction structures in deep-marine bottom-current reworked sands in the Pliocene and Pleistocene,Gulf of Mexico,Geology,1993.
[9]
Shanmugam G,50 years of the turbidite paradigm(1950s ~1990s)deep-water processes and facies models.a critical perspective,Marine and Petroleum Geology,2000.
[10]
Shanmugam G,Deep-marine tidal bottom currents and their reworked sands in modern and ancient submarine canyons,Marine and Petroleum Geology,2003.
[11]
Stow D A V;Faugères J C;Howe J A;Pudsey C J,Viana A R,Bottom currents,contourites and deep-sea sediment drifts:current state-of-the-art,London:Geological Society,Memoirs,2002.
[12]
Viana A R;Almeida J W;Machado L C,Different styles of canyon infill related to gravity and bottom current processes:Example from the upper slope of the SE Brazilian margin,Publica ao Sexto Congresso International da Sociedade Brasileira de Geofisica,SBGF 014,4,1999.
Zhu Mangzheng;Graham S;Pang Xiong;McHargue T,Characteristics of migrating submarine canyons from the middle Miocene to present:Implications for paleoceanograpic circulation,northern South China Sea,Marine and Petroleum Geology,2010.
Flavio S.Anselmetti ;Gregor P.Eberli ;Zan-Dong Ding,Form the Great Bahama Bank into the Straits of Florida: A margin architecture controlled by sea-level fluctuations adn ocean currents,Geological Society of America Bulletin?,2000, 112(6).
[25]
Armishaw J E;Holmes R;Stow D A V,Hebrides slope apron and Barra fan,NW UK continental margin sedimentation,London:Geological Society Special Publications,1998.
[26]
Armishaw J E;Holmes R W;Stow D A V,The Barra Fan:a bottom-current reworked,glacially-fed submarine fan system,Marine and Petroleum Geology,2000.
[27]
Damuth J E,Migrating sediment waves created by turbidity currents in the northern South China Basin,Geology,1979.
[28]
Faugères J C;Mwzerais M L;Stow D A V,Contourite drift types and their distribution in the North and South Atlantic Ocean Basins,Sedimentary Geology,1993.
[29]
Faugères J C;Stow D A V,Bottom-currents-controlled sedimentation:a synthesis of the contourite problem,Sedimentary Geology,1993.
[30]
J.-C. Faugères ;D. A. V. Stow,Seismic features diagnostic of contourite drifts,Marine Geology?,1999, 162(1).
[31]
Gong Chenglin;Wang Yingmiu;Peng Xuechao;Li Weiguo Qiu Yan Xu Shang,Sediment waves on the South China Sea Slope off southwestern Taiwan:Implications for the intrusion of the Northern Pacific Deep Water into the South China Sea,Marine and Petroleum Geology,2012.
[32]
He Yunlong;Xie Xinong;Benjamin C;Kneller,Wang Zhenfeng,Li Xushen,Architecture and controlling factors of canyon fills on the shelf margin in the Qiongdongnan Basin,northern South China Sea,Marine and Petroleum Geology,2012.
[33]
K(a)hler G;Stow D A V,Turbidites and contourites of the Palaeogene Lefkara Formation,southern Cyprus,Sedimentary Geology,1998.
[34]
Kuvaas B;Leitchenkov G,Glaciomarine turbidite and current controlled deposits in Prydz Bay,Antarctica,Marine Geology,1992(3-4).
[35]
Kuvaas B;Kristoffersen Y;Guseva J;Leitchenkov G Gandjukhin V L(φ)v(a)s O Sand M Brekke H,Interplay of turbidite and contourite deposition along the Cosmonaut Sea/Enderby Land margin,East Antarctica,Marine Geology,2005.
[36]
Liu Zhifei;Colin C;Li Xiajing;Zhao Yulong Tuo Shouting Chen Zhong Siringan F P Liu J T Huang Chiyue You Chenfeng Huang Kuofang,Clay mineral distribution in surface sediments of the northeastern South China Sea and surrounding fluvial drainage basins:Source and transport,Marine Geology,2010(1 -4).
[37]
Lüdmann T;Wong H K;Berglar K,Upward flow of North Pacific Deep Water in the northern South China Sea as deduced from the occurrence of drift sediments,Geophysical Research Letters,2005.
[38]
Marchèès E;Mulder T;Cremer M;Bonnel C Hanquiez V Gonthier E Lecroart P,Contourite drift construction influenced by capture of Mediterranean Outflow Water deep-sea current by the Portim(ā)o submarine canyon(Gulf of Cadiz,South Portugal),Marine Geology,2007.
[39]
Massé L;Faugères J C;Hrovatin V,The interplay between turbidity and contour processes on the Columbia Channel fan drift,Southern Brazil Basin,Sedimentary Geology,1998.
[40]
Mulder T;Lecroart P;Hanquiez V;Marches E Gonthier E Guedes J C Thiébot E Jaaidi B Kenyon N Voisset M Perez C Sayago M Fuchey Y Bujan S,The western part of the Gulf of Cadiz:contour currents and turbidity currents interactions,Geo-Marine Letters,2006.
Rasmussen S;Lykke-Andersen H;Kuijpers A,Post-Miocene sedimentation at the continental rise of Southeast Greenland:the interplay between turbidity and contour currents,Marine Geology,2003.
[43]
Reed D L;Meyer A W;Silver E A;Prasetyo H,Contourite sedimentation in an intraoceanic forearc system:eastern Sunda Arc,Indonesia,Marine Geology,1987(3 - 4).