[1] Sømme T O, Helland-Hansen W, Martinsen O J, et al. Relationships between morphological and sedimentological parameters in source-to-sink systems: A basis for predicting semi-quantitative Characteristics in subsurface systems[J]. Basin Research, 2009, 21(4): 361-387.
[2] Gong C L, Steel R J, Wang Y M, et al. Shelf-margin architecture variability and its role in sediment-budget partitioning into deep-water areas[J]. Earth-Science Reviews, 2016, 154: 72-101.
[3] Weger W D, Hernández-Molina F J, Flecker R, et al. Late Miocene contourite channel system reveals intermittent overflow behavior[J]. Geology, 2020, 48: 1194-1199.
[4] Wang Z, Fan R Y, Zong R W, et al. Middle Ordovician bottom current deposits in the western margin of the North China Craton: Evidence from sedimentary and magnetic fabrics[C]. Sedimentology, 2022,69(3):1424-1455.
[5] Counts J W, Amy L, Georgiopoulou A, et al. A review of sand detachment in modern deep marine environments: Analogues for upslope stratigraphic traps[J]. Marine and Petroleum Geology, 2021, 132: 105184.
[6] Mayall M, Jones E, Casey M. Turbidite channel reservoirs: Key elements in facies prediction and effective development[J]. Marine and Petroleum Geology, 2006, 23(8): 821-841.
[7] Kane I A, Clare M A, Miramontes E, et al. Seafloor microplastic hotspots controlled by deep-sea circulation[J]. Science, 2020, 368(6495): 1140-1145.
[8] Reading H G, Richards M. Turbidite systems in deep-water basin margins classified by grain size and feeder system[J]. AAPG Bulletin, 1994, 78(5): 792-822.
[9] Stow D A V, Mayall M. Deep-water sedimentary systems: New models for the 21st century[J]. Marine and Petroleum Geology, 2000, 17(2): 125-135.
[10] Heezen B C, Hollister C D. Deep sea current evidence from abyssal sediments[J]. Marine Geology, 1964, 1: 141-174.
[11] Michels K H, Rogenhagen J, Kuhn G. Recognition of contour-current influence in mixed contourite-turbidite sequences of the western Weddell Sea, Antarctica[J]. Marine Geophysical Researches, 2001, 22(5/6): 465-485.
[12] Rasmussen S, Lykke-Andersen H, Kuijpers A, et al. Post-Miocene sedimentation at the continental rise of Southeast Greenland: The interplay between turbidity and contour currents[J]. Marine Geology, 2003, 196(1/2): 37-52.
[13] Salles T, Marchès E, Dyt C, et al. Simulation of the interactions between gravity processes and contour currents on the Algarve Margin (South Portugal) using the stratigraphic forward model Sedsim[J]. Sedimentary Geology, 2010, 229(3): 95-109.
[14] Mulder T, Faugères J C, Gonthier E. Mixed turbidite-contourite Systems[M]//Ainsley M, Ashworth P J, Best J L, et al. Developments in sedimentology. Amsterdam: Elsevier, 2008: 435-456.
[15] 李华,王英民,徐强,等. 南海北部珠江口盆地重力流与等深流交互作用沉积特征、过程及沉积模式[J]. 地质学报,2014,88(6):1120-1129.

Li Hua, Wang Yingmin, Xu Qiang, et al. Interactions between down-slope and along-slope processes on the northern slope of South China Sea: Products, processes, and depositional model[J]. Acta Geologica Sinica, 2014, 88(6): 1120-1129.
[16] Hsü K J. Cross-laminations in graded bed sequences[J]. Journal of Sedimentary Research, 1964, 34(2): 379-388.
[17] Hubert J F. Textural evidence for deposition of many western North Atlantic deep-sea sands by ocean-bottom currents rather than turbidity currents[J]. The Journal of Geology, 1964, 72(6): 757-785.
[18] Lovell J P B, Stow D A W. Identification of ancient sandy contourites[J]. Geology, 1981, 9(8): 347-349.
[19] Alonso B, Ercilla G, Casas D, et al. Contourite vs gravity-flow deposits of the Pleistocene faro drift (gulf of Cadiz): Sedimentological and mineralogical approaches[J]. Marine Geology, 2016, 377: 77-94.
[20] Ercilla G, Juan C, Periáñez R, et al. Influence of alongslope processes on modern turbidite systems and canyons in the Alboran Sea (southwestern Mediterranean)[J]. Deep Sea Research Part I: Oceanographic Research Papers, 2019, 144: 1-16.
[21] Gauchery T, Rovere M, Pellegrini C, et al. Post-LGM multi-proxy sedimentary record of bottom-current variability and downslope sedimentary processes in a contourite drift of the Gela Basin (Strait of Sicily)[J]. Marine Geology, 2021, 439: 106564.
[22] Marchès E, Mulder T, Gonthier E, et al. Perched lobe formation in the Gulf of Cadiz: Interactions between gravity processes and contour currents (Algarve Margin, southern Portugal)[J]. Sedimentary Geology, 2010, 229(3): 81-94.
[23] Mencaroni D, Urgeles R, Camerlenghi A, et al. A mixed turbidite-contourite system related to a major submarine canyon: The Marquês de Pombal Drift (south-west Iberian margin)[J]. Sedimentology, 2021, 68(5): 2069-2096.
[24] Mulder T, Lecroart P, Hanquiez V, et al. The western part of the Gulf of Cadiz: Contour currents and turbidity currents interactions[J]. Geo-Marine Letters, 2006, 26(1): 31-41.
[25] van Rooij D, Iglesias J, Hernández-Molina F J, et al. The Le Danois Contourite depositional system: Interactions between the Mediterranean outflow water and the Upper Cantabrian slope (North Iberian margin)[J]. Marine Geology, 2010, 274(1/2/3/4): 1-20.
[26] Saller A H, Noah J T, Ruzuar A P, et al. Linked lowstand delta to basin-floor fan deposition, offshore Indonesia: An analog for deep-water reservoir systems[J]. AAPG Bulletin, 2004, 88(1): 21-46.
[27] Gonthier E, Faugères J C, Viana A, et al. Upper Quaternary deposits on the Sao Tomé deep-sea channel levee system (South Brazilian Basin): Major turbidite versus contourite processes[J]. Marine Geology, 2003, 199(1/2): 159-180.
[28] Massé L, Faugères J C, Hrovatin V. The interplay between turbidity and contour current processes on the Columbia Channel fan drift, southern Brazil Basin[J]. Sedimentary Geology, 1998, 115(1/2/3/4): 111-132.
[29] Pandolpho B T, Da Fontoura Klein A H, Dutra I, et al. Seismic record of a cyclic turbidite-contourite system in the northern Campos Basin, SE Brazil[J]. Marine Geology, 2021, 434: 106422.
[30] Georgiopoulou A, Owens M, Haughton P D W. Channel and inter-channel morphology resulting from the long-term interplay of alongslope and downslope processes, NE Rockall Trough, NE Atlantic[J]. Marine Geology, 2021, 441: 106624.
[31] Gong C L, Wang Y M, Rebesco M, et al. How do turbidity flows interact with contour currents in unidirectionally migrating deep-water channels?[J]. Geology, 2018, 46(6): 551-554.
[32] Li W, Li S, Alves T M, et al. The role of sediment gravity flows on the morphological development of a large submarine canyon (Taiwan Canyon), north-east South China Sea[J]. Sedimentology, 2021, 68(3): 1091-1108.
[33] Li H, Wang Y M, Zhu W L, et al. Seismic characteristics and processes of the Plio-Quaternary unidirectionally migrating channels and contourites in the northern slope of the South China Sea[J]. Marine and Petroleum Geology, 43: 370-380.
[34] Wang X X, Zhuo H T, Wang Y M, et al. Controls of contour currents on intra-canyon mixed sedimentary processes: Insights from the Pearl River Canyon, northern South China Sea[J]. Marine Geology, 2018, 406: 193-213.
[35] Kenyon N H, Akhmetzhanov A M, Twichell D C. Sand wave fields beneath the Loop Current, Gulf of Mexico: Reworking of fan sands[J]. Marine Geology, 192(1/2/3): 297-307.
[36] Kuvaas B, Kristoffersen Y, Guseva J, et al. Interplay of turbidite and contourite deposition along the Cosmonaut Sea/Enderby Land margin, East Antarctica[J]. Marine Geology, 2005, 217(1/2): 143-159.
[37] Lobo F J, López-Quirós A, Hernández-Molina F J, et al. Recent morpho-sedimentary processes in Dove Basin, southern Scotia Sea, Antarctica: A basin-scale case of interaction between bottom currents and mass movements[J]. Marine Geology, 2021, 441: 106598.
[38] Miramontes E, Thiéblemont A, Babonneau N, et al. Contourite and mixed turbidite-contourite systems in the Mozambique Channel (SW Indian Ocean): Link between geometry, sediment characteristics and modelled bottom currents[J]. Marine Geology, 2021, 437: 106502.
[39] Mosher D C, Campbell D C, Gardner J V, et al. The role of deep-water sedimentary processes in shaping a continental margin: The Northwest Atlantic[J]. Marine Geology, 2017, 393: 245-259.
[40] Normandeau A, Campbell D C, Cartigny M J B. The influence of turbidity currents and contour currents on the distribution of deep-water sediment waves offshore eastern Canada[J]. Sedimentology, 2019, 66(5): 1746-1767.
[41] de Castro S, Hernández-Molina F J, Rodríguez-Tovar F J, et al. Contourites and bottom current reworked sands: Bed facies model and implications[J]. Marine Geology, 2020, 428: 106267.
[42] Fonnesu M, Palermo D, Galbiati M, et al. A new world-class deep-water play-type, deposited by the syndepositional interaction of turbidity flows and bottom currents: The giant Eocene Coral Field in northern Mozambique[J]. Marine and Petroleum Geology, 2020, 111: 179-201.
[43] Fuhrmann A, Kane I A, Clare M A, et al. Hybrid turbidite-drift channel complexes: An integrated multiscale model[J]. Geology, 2020, 48(6): 562-568.
[44] Luan X W, Lu Y T, Fan G Z, et al. Deep-water sedimentation controlled by interaction between bottom current and gravity flow: A case study of Rovuma Basin, East Africa[J]. Journal of African Earth Sciences, 2021, 180: 104228.
[45] Sansom P. Hybrid turbidite-contourite systems of the Tanzanian margin[J]. Petroleum Geoscience, 2018, 24(3): 258-276.
[46] Gong C L, Wang Y M, Zheng R C, et al. Middle Miocene reworked turbidites in the Baiyun Sag of the Pearl River Mouth Basin, northern South China Sea margin: Processes, genesis, and implications[J]. Journal of Asian Earth Sciences, 2016, 128: 116-129.
[47] Gong C L, Wang Y M, Zhu W L, et al. Upper Miocene to Quaternary unidirectionally migrating deep-water channels in the Pearl River Mouth Basin, northern South China Sea[J]. AAPG Bulletin, 2013, 97(2): 285-308.
[48] Zhu M Z, Graham S, Pang X, et al. Characteristics of migrating submarine canyons from the Middle Miocene to present: Implications for paleoceanographic circulation, northern South China Sea[J]. Marine and Petroleum Geology, 2010, 27(1): 307-319.
[49] Zhou W, Wang Y M, Gao X Z, et al. Architecture, evolution history and controlling factors of the Baiyun submarine canyon system from the Middle Miocene to Quaternary in the Pearl River Mouth Basin, northern South China Sea[J]. Marine and Petroleum Geology, 2015, 67: 389-407.
[50] He Y L, Xie X N, Kneller B C, et al. Architecture and controlling factors of canyon fills on the shelf margin in the Qiongdongnan Basin, northern South China Sea[J]. Marine and Petroleum Geology, 2013, 41: 264-276.
[51] 黄银涛,姚光庆,朱红涛,等. 莺歌海盆地东方区黄流组重力流砂体的底流改造作用[J]. 石油学报,2016,37(7):855-866.

Huang Yintao, Yao Guangqing, Zhu Hongtao, et al. Reworking of gravity flow sandbody by bottom-current from Huangliu Formation in Dongfang area of Yinggehai Basin, northwestern South China Sea[J]. Acta Petrolei Sinica, 2016, 37(7): 855-866.
[52] 李俞锋,蒲仁海,唐明,等. 一种新型底流与浊流交互作用形成的储集砂体:以北礁凹陷为例[J]. 岩性油气藏,2018,30(6):55-66.

Li Yufeng, Pu Renhai, Tang Ming, et al. A new reservoir sand body resulted from interaction between turbidity flows and bottom currents: A case from Beijiao Sag of Qiongdongnan Basin[J]. Lithologic Reservoirs, 2018, 30(6): 55-66.
[53] 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[J]. AAPG Bulletin, 1993, 77(7): 1241-1259.
[54] Anketell J M, Lovell J P B. Upper Llandoverian Grogal sandstones and Aberystwyth grits in the New Quay area, central wales: A possible upwards transition from contourites to turbidites[J]. Geological Journal, 1976, 11(2): 101-108.
[55] Bein A, Weiler Y. The Cretaceous Talme Yafe Formation: A contour current shaped sedimentary prism of calcareous detritus at the continental margin of the Arabian Craton[J]. Sedimentology, 1976, 23(4): 511-532.
[56] Hovikoski J, Uchman A, Weibel R, et al. Upper Cretaceous bottom current deposits, north-east Greenland[J]. Sedimentology, 2020, 67(7): 3619-3654.
[57] Hüneke H, Hernández-Molina F J, Rodríguez-Tovar F J, et al. Diagnostic criteria using microfacies for calcareous contourites, turbidites and pelagites in the Eocene-Miocene slope succession, southern Cyprus[J]. Sedimentology, 2021, 68(2): 557-592.
[58] Kähler G, Stow D A V. Turbidites and contourites of the Palaeogene Lefkara Formation, southern Cyprus[J]. Sedimentary Geology, 1998, 115(1/2/3/4): 215-231.
[59] Rodrigues S, Hernández-Molina F J, Kirby A. A Late Cretaceous mixed (turbidite-contourite) system along the Argentine margin: Paleoceanographic and conceptual implications[J]. Marine and Petroleum Geology, 2021, 123: 104768.
[60] Stanley D J. Model for turbidite-to-contourite continuum and multiple process transport in deep marine settings: Examples in the rock record[J]. Sedimentary Geology, 1993, 82(1/2/3/4): 241-255.
[61] De Weger W, Hernández-Molina F J, Miguez-Scalas O, et al. Contourite depositional system after the exit of a strait: Case study from the Late Miocene South Rifian Corridor, Morocco[J]. Sedimentology, 2021, 68(7): 2996-3032.
[62] Ito M. Sandy contourites of the Lower Kazusa group in the Boso Peninsula, Japan; Kuroshio-current-influenced deep-sea sedimentation in a Plio-Pleistocene Forearc Basin[J]. Journal of Sedimentary Research, 1996, 66(3): 587-598.
[63] 李华,何幼斌. 鄂尔多斯盆地西南缘奥陶系平凉组改造砂沉积特征及意义[J]. 石油与天然气地质,2018,39(2):384-397.

Li Hua, He Youbin. Sedimentary characteristics and significance of reworked sands in the Ordovician Pingliang Formation, southwestern margin of Ordos Basin[J]. Oil & Gas Geology, 2018, 39(2): 384-397.
[64] Li H, van Loon A J, He Y B. Interaction between turbidity currents and a contour current-A rare example from the Ordovician of Shaanxi province, China[J]. Geologos, 2019, 25(1): 15-30.
[65] Li H, van Loon A J, He Y B. Cannibalism of contourites by gravity flows: Explanation of the facies distribution of the Ordovician Pingliang Formation along the southern margin of the Ordos Basin, China[J]. Canadian Journal of Earth Sciences, 2020, 57(3): 331-347.
[66] Li H, Zhao H Y, Xu Y X, et al. Characteristics of debrites, turbidites, and contourites in the Upper Ordovician Pingliang Formation along southwestern margin of the Ordos Basin, western China[J]. Arabian Journal of Geosciences, 2021, 14(17): 1730.
[67] Li H, van Loon A J, He Y B. When turbidity currents cross contour currents: A struggle for life in the Ordovician along the southern margin of the Ordos Basin (China)[M]//Yang R C, van Loon A J. The Ordos Basin: Sedimentological research for hydrocarbons exploration. Amsterdam: Elsevier, 2022: 269-285.
[68] Wang Z, Fan R Y, Zong R W, et al. Composition and spatiotemporal evolution of the mixed turbidite-contourite systems from the Middle Ordovician, in western margin of the North China Craton[J]. Sedimentary Geology, 2021, 421: 105943.
[69] Stow D, Smillie Z. Distinguishing between deep-water sediment facies: Turbidites, contourites and hemipelagites[J]. Geosciences, 2020, 10(2): 68.
[70] 吴嘉鹏,王英民,王海荣,等. 深水重力流与底流交互作用研究进展[J]. 地质论评,2012,58(6):1110-1120.

Wu Jiapeng, Wang Yingmin, Wang Hairong, et al. The interaction between deep-water turbidity and bottom currents: A review[J]. Geological Review, 2012, 58(6): 1110-1120.
[71] Middleton G V, Hampton M A. Sediment gravity flows: Mechanics of flow and deposition[M]//Middleton G V, Bouma A H. Turbidites and deepwater sedimentation. Los Angeles: Society of Economic Paleontologists and Mineralogists, 1973: 1-38.
[72] 何幼斌,王文广. 沉积岩与沉积相[M]. 2版. 北京:石油工业出版社,2017:301-311.

He Youbin, Wang Wenguang. Sedimentary rock and facies[M]. 2nd ed. Beijing: Petroleum Industry Press, 2017: 301-311.
[73] Slootman A, Cartigny M J B. Cyclic steps: Review and aggradation-based classification[J]. Earth-Science Reviews, 2020, 201: 102949.
[74] Zavala C. Hyperpycnal (over density) flows and deposits[J]. Journal of Palaeogeography, 2020, 9(3): 267-287.
[75] Ono K, Plink-Björklund P. Froude supercritical flow bedforms in deepwater slope channels? Field examples in conglomerates, sandstones and fine-grained deposits[J]. Sedimentology, 2018, 65(3): 639-669.
[76] 杨仁超,金之钧,孙冬胜,等. 鄂尔多斯晚三叠世湖盆异重流沉积新发现[J]. 沉积学报,2015,33(1):10-20.

Yang Renchao, Jin Zhijun, Sun Dongsheng, et al. Discovery of hyperpycnal flow deposits in the Late Triassic lacustrine Ordos Basin[J]. Acta Sedimentologica Sinica, 2015, 33(1): 10-20.
[77] 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.
[78] 操应长,杨田,王艳忠,等. 超临界沉积物重力流形成演化及特征[J]. 石油学报,2017,38(6):607-621.

Cao Yingchang, Yang Tian, Wang Yanzhong, et al. Formation, evolution and sedimentary characteristics of supercritical sediment gravity-flow[J]. Acta Petrolei Sinica, 2017, 38(6): 607-621.
[79] Stow D A V, Pudsey C J, Howe J A, et al. Deep-water contourite systems: Modern drifts and ancient series, seismic and sedimentary characteristics[M]. London: The Geological Society, 2002.
[80] Stow D A V, Lovell J P B. Contourites: Their recognition in modern and ancient sediments[J]. Earth-Science Reviews, 1979, 14(3): 251-291.
[81] Faugères J C, Stow D A V, Imbert P, et al. Seismic features diagnostic of contourite drifts[J]. Marine Geology, 1999, 162(1): 1-38.
[82] Rebesco M, Hernández-Molina F J, van Rooij D, et al. Contourites and associated sediments controlled by deep-water circulation processes: State-of-the-art and future considerations[J]. Marine Geology, 2014, 352: 111-154.
[83] Stow D A V, Faugères J C. Contourite facies and the facies model[M]//Rebesco M, Camerlenghi A. Developments in sedimentology. Amsterdam: Elsevier, 2008: 223-256.
[84] 李华,何幼斌,黄伟,等. 鄂尔多斯盆地南缘奥陶系平凉组等深流沉积[J]. 古地理学报,2016,18(4):631-642.

Li Hua, He Youbin, Huang Wei, et al. Contourites of the Ordovician Pingliang Formation in southern margin of Ordos Basin[J]. Journal of Palaeogeography, 2016, 18(4): 631-642.
[85] 高振中. 深水牵引流沉积:内潮汐、内波和等深流沉积研究[M]. 北京:科学出版社,1996:47-86.

Gao Zhenzhong. Deep-water tractive current deposits: The study of internal-tide, internal-wave, and contour current deposits[M]. Beijing: Science Press, 1996: 47-86.
[86] Nielsen T, Knutz P C, Kuijpers A. Seismic expression of contourite depositional systems[M]//Rebesco M, Camerlenghi A. Developments in sedimentology. Amsterdam: Elsevier, 2008: 301-321.
[87] Stow D A V, Faugères J C, Viana A, et al. Fossil contourites: A critical review[J]. Sedimentary Geology, 1998, 115(1/2/3/4): 3-31.
[88] Hüneke H, Stow D A V. Identification of ancient contourites: Problems and palaeoceanographic significance[M]//Rebesco M, Camerlenghi A. Developments in sedimentology. Amsterdam: Elsevier, 2008: 323-344.
[89] Shanmugam G. Deep-marine tidal bottom currents and their reworked sands in modern and ancient submarine canyons[J]. Marine and Petroleum Geology, 2003, 20(5): 471-491.
[90] Shanmugam G. Deep-water bottom currents and their deposits[M]//Rebesco M, Camerlenghi A. Developments in sedimentology. Amsterdam: Elsevier, 2008: 59-81.
[91] Campbell D C, Mosher D C. Geophysical evidence for widespread Cenozoic bottom current activity from the continental margin of Nova Scotia, Canada[J]. Marine Geology, 2016, 378: 237-260.
[92] Lu Y T, Luan X W, Shi B Q, et al. Migrated hybrid turbidite-contourite channel-lobe complex of the Late Eocene Rovuma Basin, East Africa[J]. Acta Oceanologica Sinica, 2021, 40(2): 81-94.
[93] Hernández-Molina F J, Llave E, Stow D A V. Continental slope contourites[M]//Rebesco M, Camerlenghi A. Developments in sedimentology. Amsterdam: Elsevier, 2008: 379-408.
[94] 周伟. 深水单向迁移水道建造模式与成因机制研究进展[J]. 古地理学报,2021,23(6):1082-1093.

Zhou Wei. Research progress on architectural patterns and formation mechanisms of deep-water unidirectionally migrating channels[J]. Journal of Palaeogeography, 2021, 23(6): 1082-1093.
[95] Chen Y H, Yao G S, Wang X F, et al. Flow processes of the interaction between turbidity flows and bottom currents in sinuous unidirectionally migrating channels: An example from the Oligocene channels in the Rovuma Basin, offshore Mozambique[J]. Sedimentary Geology, 2020, 404: 105680.
[96] Miramontes E, Eggenhuisen J T, Jacinto R S, et al. Channel-levee evolution in combined contour current-turbidity current flows from flume-tank experiments[J]. Geology, 2020, 48(4): 353-357.
[97] 张功成,屈红军,赵冲,等. 全球深水油气勘探40年大发现及未来勘探前景[J]. 天然气地球科学,2017,28(10):1447-1477.

Zhang Gongcheng, Qu Hongjun, Zhao Chong, et al. Giant discoveries of oil and gas exploration in global deepwaters in 40 years and the prospect of exploration[J]. Natural Gas Geoscience, 2017, 28(10): 1447-1477.
[98] Viana A R, Almeida W, Nunes M C V, et al. The economic importance of contourites[M]//Viana A R, Rebesco M. Economic and palaeoceanographic significance of contourite deposits. London: The Geological Society, 2007: 1-24.
[99] Yu X H, Stow D, Smillie Z, et al. Contourite porosity, grain size and reservoir characteristics[J]. Marine and Petroleum Geology, 2020, 117: 104392.
[100] Bailey W, McArthur A, McCaffrey W. Sealing potential of contourite drifts in deep-water fold and thrust belts: Examples from the Hikurangi margin, New Zealand[J]. Marine and Petroleum Geology, 2021, 123: 104776.
[101] Hernández-Molina F J, Soto M, Piola A R, et al. A contourite depositional system along the Uruguayan continental margin: Sedimentary, oceanographic and paleoceanographic implications[J]. Marine Geology, 2016, 378: 333-349.
[102] 李华,何幼斌. 等深流沉积研究进展[J]. 沉积学报,2017,35(2):228-240.

Li Hua, He Youbin. Research processes on contourites[J]. Acta Sedimentologica Sinica, 2017, 35(2): 228-240.
[103] Knutz P C. Palaeoceanographic significance of contourite drifts[M]//Rebesco M, Camerlenghi A. Developments in sedimentology. Amsterdam: Elsevier, 2008: 511-535.
[104] 李华,何幼斌,黄伟,等. 鄂尔多斯盆地南缘奥陶系平凉组深水沉积特征及其与古环境关系:以陕西富平赵老峪地区为例[J]. 沉积学报,2018,36(3):483-499.

Li Hua, He Youbin, Huang Wei, et al. Research on relationship between characteristics of deep-water deposits and palaeoenvironment in the Ordovician, Pingliang Formation, southern margin of the Ordos Basin: A case of Zhaolaoyu countryside, Fuping town, Shaanxi province[J]. Acta Sedimentologica Sinica, 2018, 36(3): 483-499.
[105] 孙启良,解习农,吴时国. 南海北部海底滑坡的特征、灾害评估和研究展望[J]. 地学前缘,2021,28(2):258-270.

Sun Qiliang, Xie Xinong, Wu Shiguo. Submarine landslides in the northern South China Sea: Characteristics, geohazard evaluation and perspectives[J]. Earth Science Frontiers, 2021, 28(2): 258-270.
[106] 周庆杰,李西双,徐元芹,等. 一种基于水深梯度原理的海底滑坡快速识别方法:以南海北部陆坡白云深水区为例[J]. 海洋学报,2017,39(1):138-147.

Zhou Qingjie, Li Xishuang, Xu Yuanqin, et al. A rapid method to recognize submarine landslides based on the principle of water depth gradient: A case of Baiyun deep-water area, north slope of the South China Sea[J]. Haiyang Xuebao, 2017, 39(1): 138-147.
[107] 马云,李三忠,梁金强,等. 南海北部琼东南盆地海底滑坡特征及其成因机制[J]. 吉林大学学报(地球科学版),2012,42(增刊3):196-205.

Ma Yun, Li Sanzhong, Liang Jinqiang, et al. Characteristics and mechanism of submarine landslides in the Qiongdongnan Basin, northern South China Sea[J]. Journal of Jilin University (Earth Science Edition), 2012, 42(Suppl.3): 196-205.
[108] 孙运宝,吴时国,王志君,等. 南海北部白云大型海底滑坡的几何形态与变形特征[J]. 海洋地质与第四纪地质,2008,28(6):69-77.

Sun Yunbao, Wu Shiguo, Wang Zhijun, et al. The geometry and deformation characteristics of Baiyun submarine landslide[J]. Marine Geology & Quaternary Geology, 2008, 28(6): 69-77.
[109] Miramontes E, Garziglia S, Sultan N, et al. Morphological control of slope instability in contourites: A geotechnical approach[J]. Landslides, 2018, 15(6): 1085-1095.
[110] Masson D G, Watts A B, Gee M J R, et al. Slope failures on the flanks of the western Canary Islands[J]. Earth-Science Reviews, 2002, 57(1/2): 1-35.
[111] Sultan N, Cochonat P, Canals M, et al. Triggering mechanisms of slope instability processes and sediment failures on continental margins: A geotechnical approach[J]. Marine Geology, 2004, 213(1/2/3/4): 291-321.