[1] Wynn R B, Huvenne V A I, Le Bas T P, et al. Autonomous underwater vehicles （AUVs）： Their past, present and future contributions to the advancement of marine geoscience[J]. Marine Geology, 2014, 352： 451-468.
[2] Clift P, Gaedicke C. Accelerated mass flux to the Arabian Sea during the Middle to Late Miocene[J]. Geology, 2002, 30（3）： 207-210.
[3] Covault J A, Romans B W, Fildani A, et al. Rapid climatic signal propagation from source to sink in a southern California sediment-routing system[J]. The Journal of Geology, 2010, 118（3）： 247-259.
[4] Pettingill H S, Weimer P. Worlwide deepwater exploration and production： Past, present, and future[J]. The Leading Edge, 2002, 21（4）： 371-376.
[5] Talling P J, Allin J, Armitage D A, et al. Key future directions for research on turbidity currents and their deposits[J]. Journal of Sedimentary Research, 2015, 85（2）： 153-169.
[6] Flood R D, Shor A N. Mud waves in the Argentine Basin and their relationship to regional bottom circulation patterns[J]. Deep Sea Research Part A. Oceanographic Research Papers, 1988, 35（6）： 943-971.
[7] Piper D J W, Savoye B. Processes of Late Quaternary turbidity current flow and deposition on the Var Deep-Sea fan, North-West Mediterranean sea[J]. Sedimentology, 1993, 40（3）： 557-582.
[8] Wynn R B, Stow D A V. Classification and characterisation of deep-water sediment waves[J]. Marine Geology, 2002, 192（1/2/3）： 7-22.
[9] Gong C L, Wang Y M, Peng X C, et al. 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[J]. Marine and Petroleum Geology, 2012, 32（1）： 95-109.
[10] Covault J A, Kostic S, Paull C K, et al. Submarine channel initiation, filling and maintenance from sea-floor geomorphology and morphodynamic modelling of cyclic steps[J]. Sedimentology, 2014, 61（4）： 1031-1054.
[11] Kostic S, Parker G. The response of turbidity currents to a canyon-fan transition： Internal hydraulic jumps and depositional signatures[J]. Journal of Hydraulic Research, 2006, 44（5）： 631-653.
[12] Postma G, Cartigny M J B. Supercritical and subcritical turbidity currents and their deposits-A synthesis[J]. Geology, 2014, 42（11）： 987-990.
[13] Bouma A H. Sedimentology of some flysch deposits： A graphic approach to facies interpretation[M]. Amsterdam： Elsevier, 1962： 168.
[14] Heerema C J, Talling P J, Cartigny M J, et al. What determines the downstream evolution of turbidity currents?[J]. Earth and Planetary Science Letters, 2020, 532： 116023.
[15] Symons W O, Sumner E J, Talling P J, et al. Large-scale sediment waves and scours on the modern seafloor and their implications for the prevalence of supercritical flows[J]. Marine Geology, 2016, 371： 130-148.
[16] Paull C K, Ussler III W, Caress D W, et al. Origins of large crescent-shaped bedforms within the axial channel of Monterey Canyon, offshore California[J]. Geosphere, 2010, 6（6）： 755-774.
[17] Babonneau N, Delacourt C, Cancouët R, et al. Direct sediment transfer from land to deep-sea： Insights into shallow multibeam bathymetry at La Réunion Island[J]. Marine Geology, 2013, 346： 47-57.
[18] Arzola R G, Wynn R B, Lastras G, et al. Sedimentary features and processes in the Nazaré and Setúbal submarine canyons, west Iberian margin[J]. Marine Geology, 2008, 250（1/2）： 64-88.
[19] 李全,吴伟,康洪全,等. 西非下刚果盆地深水水道沉积特征及控制因素[J]. 石油与天然气地质,2019,40（4）：917-929.

Li Quan, Wu Wei, Kang Hongquan, et al. Characteristics and controlling factors of deep-water channel sedimentation in Lower Congo Basin, West Africa[J]. Oil & Gas Geology, 2019, 40（4）： 917-929.
[20] Shepard F P. Submarine canyons： Multiple causes and long-time persistence[J]. AAPG Bulletin, 1981, 65（6）： 1062-1077.
[21] Normark W R. Growth patterns of deep-sea fans[J]. AAPG Bulletin, 1970, 54（11）： 2170-2195.
[22] Normark W R, Carlson P R. Giant submarine canyons： Is size any clue to their importance in the rock record?[M]//Chan M A, Archer A W. Extreme depositional environments： Mega end members in geologic time. Geological Society of America, 2003： 175-190.
[23] Smith P A. Submarine topography off the California coast： Canyons and tectonic interpretation by Francis P. Shepard, K. O. Emery[J]. Geographical Review, 1942, 32（4）： 691-693.
[24] Li Q, Wu W, Liang J S, et al. Deep-water channels in the Lower Congo Basin： Evolution of the geomorphology and depositional environment during the Miocene[J]. Marine and Petroleum Geology, 2020, 115： 104260.
[25] Wu W, Li Q, Yu J, et al. The Central Canyon depositional patterns and filling process in east of Lingshui Depression, Qiongdongnan Basin, northern South China Sea[J]. Geological Journal, 2018, 53（6）： 3064-3081.
[26] Li Q, Yu S, Wu W, et al. Detection of a deep-water channel in 3D seismic data using the sweetness attribute and seismic geomorphology： A case study from the Taranaki Basin, New Zealand[J]. New Zealand Journal of Geology and Geophysics, 2017, 6（3）： 199-208.
[27] Paull C K, McGann M, Sumner E J, et al. Sub-decadal turbidite frequency during the Early Holocene： Eel Fan, offshore northern California[J]. Geology, 2014, 42（10）： 855-858.
[28] Macdonald H A, Wynn R B, Huvenne V A I, et al. New insights into the morphology, fill, and remarkable longevity （>0.2 m.y.） of modern deep-water erosional scours along the northeast Atlantic margin[J]. Geosphere, 2011, 7（4）： 845-867.
[29] Terrinha P, Matias L, Vicente J, et al. Morphotectonics and strain partitioning at the Iberia-Africa plate boundary from multibeam and seismic reflection data[J]. Marine Geology, 2009, 267（3/4）： 156-174.
[30] Fildani A, Normark W R, Kostic S, et al. Channel formation by flow stripping： Large-scale scour features along the Monterey East Channel and their relation to sediment waves[J]. Sedimentology, 2006, 53（6）： 1265-1287.
[31] Zhong G F, Cartigny M J B, Kuang Z G, et al. Cyclic steps along the South Taiwan Shoal and West Penghu submarine canyons on the northeastern continental slope of the South China Sea[J]. GSA Bulletin, 2015, 127（5/6）： 804-824.
[32] Duarte J C, Terrinha P, Rosas F M, et al. Crescent-shaped morphotectonic features in the Gulf of Cadiz （offshore SW Iberia）[J]. Marine Geology, 2010, 271（3/4）： 236-249.
[33] Armitage D A, McHargue T, Fildani A, et al. Postavulsion channel evolution： Niger Delta continental slope[J]. AAPG Bulletin, 2012, 96（5）： 823-843.
[34] Fildani A, Hubbard S M, Covault J A, et al. Erosion at inception of deep-sea channels[J]. Marine and Petroleum Geology, 2013, 41： 48-61.
[35] Rowan M G, Peel F J, Vendeville B C. Gravity-driven fold belts on passive margins[M]//McClay K R. Thrust tectonics and hydrocarbon systems. AAPG Memoir, 2004： 159-186.
[36] Collot J Y, Agudelo W, Ribodetti A, et al. Origin of a crustal splay fault and its relation to the seismogenic zone and underplating at the erosional north Ecuador-South Colombia oceanic margin[J]. Journal of Geophysical Research： Solid Earth, 2008, 113（B12）： B12102.
[37] Kostic S. Modeling of submarine cyclic steps： Controls on their formation, migration, and architecture[J]. Geosphere, 2011, 7（2）： 294-304.
[38] Smith D P, Ruiz G, Kvitek R, et al. Semiannual patterns of erosion and deposition in Upper Monterey Canyon from serial multibeam bathymetry[J]. GSA Bulletin, 2005, 117（9/10）： 1123-1133.
[39] Conway K W, Barrie J V, Picard K, et al. Submarine channel evolution： Active channels in fjords, British Columbia, Canada[J]. Geo-Marine Letters, 2012, 32（4）： 301-312.
[40] Lee H J, Syvitski J P M, Parker G, et al. Distinguishing sediment waves from slope failure deposits： Field examples, including the ‘Humboldt slide’, and modelling results[J]. Marine Geology, 2002, 192（1/2/3）： 79-104.
[41] Berndt C, Cattaneo A, Szuman M, et al. Sedimentary structures offshore Ortona, Adriatic Sea-Deformation or sediment waves?[J]. Marine Geology, 2006, 234（1/2/3/4）： 261-270.
[42] Urgeles R, De Mol B, Liquete C, et al. Sediment undulations on the Llobregat prodelta： Signs of early slope instability or sedimentary bedforms?[J]. Journal of Geophysical Research： Solid Earth, 2007, 112（B5）： B05102.
[43] Ballard J A. Structure of the lower continental rise hills of the western North Atlantic[J]. Geophysics, 1966, 31（3）： 506-523.
[44] Gardner J V, Prior D B, Field M E. Humboldt slide-A large shear-dominated retrogressive slope failure[J]. Marine Geology, 1999, 154（1/2/3/4）： 323-338.
[45] Howe J A. Turbidite and contourite sediment waves in the northern Rockall Trough, North Atlantic Ocean[J]. Sedimentology, 1996, 43（2）： 219-234.
[46] Damuth J E. Migrating sediment waves created by turbidity currents in the northern South China Basin[J]. Geology, 1979, 7（11）： 520-523.
[47] Normark W R, Hess G R, Stow D A V, et al. Sediment waves on the Monterey Fan Levee： A preliminary physical interpretation[J]. Marine Geology, 1980, 37（1/2）： 1-18.
[48] Nakajima T, Satoh M, Okamura Y. Channel-levee complexes, terminal deep-sea fan and sediment wave fields associated with the Toyama deep-sea channel system in the Japan Sea[J]. Marine Geology, 1998, 147（1/2/3/4）： 25-41.
[49] Smith D P, Kvitek R, Iampietro P J, et al. Twenty-nine months of geomorphic change in Upper Monterey Canyon （2002-2005）[J]. Marine Geology, 2007, 236（1/2）： 79-94.
[50] Migeon S, Savoye B, Faugeres J C. Quaternary development of migrating sediment waves in the Var deep-sea fan： Distribution, growth pattern, and implication for levee evolution[J]. Sedimentary Geology, 2000, 133（3/4）： 265-293.
[51] Piper D J W, Aksu A E. The source and origin of the 1929 Grand Banks turbidity current inferred from sediment budgets[J]. Geo-Marine Letters, 1987, 7（4）： 177-182.
[52] Piper D J W, Shor A N, Farre J A, et al. Sediment slides and turbidity currents on the Laurentian Fan： Sidescan sonar investigations near the epicenter of the 1929 Grand Banks earthquake[J]. Geology, 1985, 13（8）： 538-541.
[53] Piper D J W, Shor A N, Hughes Clarke J E. The 1929 “Grand Banks” earthquake, slump, and turbidity current[M]//Clifton H E. Sedimentologic consequences of convulsive geologic events. Geological Society of America, 1988： 77-92.
[54] Covault J A, Romans B W. Growth patterns of deep-sea fans revisited： Turbidite-system morphology in confined basins, examples from the California Borderland[J]. Marine Geology, 2009, 265（1/2）： 51-66.
[55] Mutti E. Distinctive thin-bedded turbidite facies and related depositional environments in the Eocene Hecho Group （south-central Pyrenees, Spain）[J]. Sedimentology, 1977, 24（1）： 107-131.
[56] Russell H A J, Arnott R W C. Hydraulic-jump and hyper concentrated-flow deposits of a glacigenic subaqueous fan： Oak Ridges moraine, southern Ontario, Canada[J]. Journal of Sedimentary Research, 2003, 73（6）： 887-905.
[57] Kostic S, Parker G. Conditions under which a supercritical turbidity current traverses an abrupt transition to vanishing bed slope without a hydraulic jump[J]. Journal of Fluid Mechanics, 2007, 586： 119-145.
[58] Xu J P, Wong F L, Kvitek R, et al. Sandwave migration in Monterey Submarine Canyon, central California[J]. Marine Geology, 2008, 248（3/4）： 193-212.
[59] Migeon S, Savoye B, Zanella E, et al. Detailed seismic-reflection and sedimentary study of turbidite sediment waves on the Var Sedimentary Ridge （SE France）： Significance for sediment transport and deposition and for the mechanisms of sediment-wave construction[J]. Marine and Petroleum Geology, 2001, 18（2）： 179-208.
[60] Wynn R B, Piper D J W, Gee M J R. Generation and migration of coarse-grained sediment waves in turbidity current channels and channel-lobe transition zones[J]. Marine Geology, 2002, 192（1/2/3）： 59-78.
[61] Embley R W, Langseth M G. Sedimentation processes on the continental rise of northeastern South America[J]. Marine Geology, 1977, 25（4）： 279-297.
[62] McHugh C M G, Ryan W B F. Sedimentary features associated with channel overbank flow： Examples from the Monterey Fan[J]. Marine Geology, 2000, 163（1/2/3/4）： 199-215.
[63] Flood R D, Shor A N, Manley P L. Morphology of abyssal mudwaves at Project MUDWAVES sites in the Argentine Basin[J]. Deep Sea Research Part II： Topical Studies in Oceanography, 1993, 40（4/5）： 859-888.
[64] Blumsack S L, Weatherly G L. Observations of the nearby flow and a model for the growth of mudwaves[J]. Deep Sea Research Part A. Oceanographic Research Papers, 1989, 36（9）： 1327-1339.
[65] Guiavarc'h C, Treguier A M, Vangriesheim A. Deep currents in the Gulf of Guinea： Along slope propagation of intraseasonal waves[J]. Ocean Science, 2009, 5（2）： 141-153.
[66] Djakouré S, Penven P, Bourlès B, et al. Respective roles of the guinea current and local winds on the coastal upwelling in the northern gulf of Guinea[J]. Journal of Physical Oceanography, 2017, 47（6）： 1367-1387.
[67] Blumsack S L. A model for the growth of mudwaves in the presence of time-varying currents[J]. Deep Sea Research Part II： Topical Studies in Oceanography, 1993, 40（4/5）： 963-974.
[68] Castro I P, Snyder W H. Experiments on wave breaking in stratified flow over obstacles[J]. Journal of Fluid Mechanics, 1993, 255： 195-211.