[1] Normark W R. Growth patterns of deep-sea fans［J］. AAPG Bulletin， 1970， 54（11）： 2170-2195.
[2] Normark W R. Fan valleys， channels， and depositional lobes on modern submarine fans： characters for recognition of sandy turbidite environments［J］. AAPG Bulletin， 1978， 62（6）： 912-931.
[3] Walker R G. Deep-water sandstone facies and ancient submarine fans： Models for exploration for stratigraphic traps［J］. AAPG Bulletin， 1978， 62（6）： 932-966.
[4] Piper D J W， Normark W R. Turbidite depositional Patterns and flow characteristics， Navy submarine fan， California borderland［J］. Sedimentology， 1983， 30（5）： 681-694.
[5] Mutti E. Turbidite systems and their relations to depositional sequences［M］//Zuffa G G. Provenance of arenites. Dordrecht： Springer， 1985： 65-93.
[6] Mutti E， Normark W R. Comparing examples of modern and ancient turbidite systems： Problems and concepts［C］//Leggett J K， Zuffa G G. Marine clastic sedimentology： Concepts and case studies. Dordrecht： Springer， 1987： 1-38.
[7] Mutti E， Normark W R. An integrated approach to the study of turbidite systems［C］//Weimer P， Link M H. Seismic facies and sedimentary processes of submarine fans and turbidite systems. New York： Springer， 1991： 75-106.
[8] Covault J A， Kostic S， Paull C K， et al. Cyclic steps and related supercritical bedforms： Building blocks of deep-water depositional systems， western North America［J］. Marine Geology， 2016，393：4-2
[9] 谈明轩，朱筱敏，刘伟，等. 旋回阶梯底形的动力地貌及其相关沉积物发育特征［J］. 地质论评，2017，63（6）：1512-1522.

Tan Mingxuan， Zhu Xiaomin， Liu Wei， et al. The morphodynamics of cyclic steps and sedimentary characteristics of associated deposits［J］. Geological Review， 2017， 63（6）： 1512-1522.
[10] Cartigny M J B， Postma G， van den Berg J H， et al. A comparative study of sediment waves and cyclic steps based on geometries， internal structures and numerical modeling［J］. Marine Geology， 2011， 280（1/2/3/4）： 40-56.
[11] 徐景平. 科学与技术并进：近20年来海底峡谷浊流观测的成就和挑战［J］. 地球科学进展，2013，28（5）：552-558.

Xu Jingping. Accomplishments and challenges in measuring turbidity currents in submarine canyons［J］. Advances in Earth Science， 2013， 28（5）： 552-558.
[12] 孙辉，唐鹏程，陈宇航，等. 东非鲁武马盆地陆坡深水沉积特征及主控因素［J］. 海洋地质与第四纪地质，2016，36（3）：59-68.

Sun Hui， Tang Pengcheng， Chen Yuhang， et al. Characteristics and controlling factors of deepwater deposits on the continental slope of the Rovuma Basin， East Africa［J］. Marine Geology & Quaternary Geology， 2016， 36（3）： 59-68.
[13] 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.
[14] 王大伟，白宏新，吴时国. 浊流及其相关的深水底形研究进展［J］. 地球科学进展，2018，33（1）：52-65.

Wang Dawei， Bai Hongxin， Wu Shiguo. The research progress of turbidity currents and related deep-water bedforms［J］. Advances in Earth Science， 2018， 33（1）： 52-65.
[15] Parker G. Some speculations on the relation between channel morphology and channel-scale flow structures［M］//Ashworth P， Bennett S J， Best J L， et al. Coherent flow structures in open channels. Chichester： John Wiley & Sons， Ltd.， 1996： 429-432.
[16] Spinewine B， Sequeiros O E， Garcia M H， et al. Experiments on wedge-shaped deep sea sedimentary deposits in minibasins and/or on channel levees emplaced by turbidity Currents. Part II. Morphodynamic evolution of the wedge and of the associated bedforms［J］. Journal of Sedimentary Research， 2009， 79（8）： 608-628.
[17] Kostic S， Sequeiros O， Spinewine B， et al. Cyclic steps： A phenomenon of supercritical shallow flow from the high mountains to the bottom of the ocean［J］. Journal of Hydro-environment Research， 2010， 3（4）： 167-172.
[18] Normandeau A， Lajeunesse P， Poiré A G， et al. Morphological expression of bedforms formed by supercritical sediment density flows on four fjord-lake deltas of the south-eastern Canadian Shield （Eastern Canada）［J］. Sedimentology， 2016， 63（7）： 2106-2129.
[19] Turmel D， Locat J， Parker G. Morphological evolution of a well-constrained， subaerial⁃subaqueous source to sink system： Wabush Lake［J］. Sedimentology， 2015， 62（6）： 1636-1664.
[20] Ventra D， Cartigny M J B， Bijkerk J F， et al. Supercritical-flow structures on a Late Carboniferous delta front： Sedimentologic and paleoclimatic significance［J］. Geology， 2015， 43（8）： 731-734.
[21] Slootman A， Cartigny M J B. Cyclic steps： Review and aggradation-based classification［J］. Earth-Science Reviews， 2019， 201： 102949.
[22] 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.
[23] Postma G， Cartigny M J B. Supercritical and subcritical turbidity currents and their deposits-A synthesis［J］. Geology， 2014， 42（11）： 987-990.
[24] 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.
[25] Wynn R B， Kenyon N H， Masson D G， et al. Characterization and recognition of deep-water channel-lobe transition zones［J］. AAPG Bulletin， 2002， 86（8）： 1441-1462.
[26] Coffin M F， Rabinowitz P D. Reconstruction of Madagascar and Africa： Evidence from the Davie Fracture Zone and western Somali Basin［J］. Journal of Geophysical Research： Solid Earth， 1987， 92（B9）： 9385-9406.
[27] Mahanjane E S， Franke D. The Rovuma Delta deep-water fold-and-thrust belt， offshore Mozambique［J］. Tectonophysics， 2014， 614： 91-99.
[28] Salazar M U， Baker D， Francis M， et al. Frontier exploration offshore the Zambezi Delta， Mozambique［J］. First Break， 2013， 31（6）： 135-144.
[29] 孙辉，吕福亮，范国章，等. 三级层序内受底流影响的富砂深水沉积演化规律：以东非鲁武马盆地中中新统为例［J］. 天然气地球科学，2017，28（1）：106-115.

Sun Hui， Fuliang Lü， Fan Guozhang， et al. Evolution of deepwater sand-rich sediments affected by bottom currents in the 3rd order sequences： A case study of Middle Miocene in the Ruvuma Basin［J］. Natural Gas Geoscience， 2017， 28（1）： 106-115.
[30] 孙辉，刘少治，马宏霞，等. 东非鲁武马盆地海底水道—朵体体系粗粒浊流沉积物波特征及主控因素［J］. 沉积学报，2017，35（4）：763-771.

Sun Hui， Liu Shaozhi， Ma Hongxia， et al. Characteristics and controlling factors of coarse-grained turbidite sediment waves in submarine channel-lobe system of the Ruvuma Basin， East Africa［J］. Acta Sedimentologica Sinica， 2017， 35（4）： 763-771.
[31] 张光亚，刘小兵，温志新，等. 东非被动大陆边缘盆地构造—沉积特征及其对大气田富集的控制作用［J］. 中国石油勘探，2015，20（4）：71-80.

Zhang Guangya， Liu Xiaobing， Wen Zhixin， et al. Structural and sedimentary characteristics of passive continental margin basins in East Africa and their effect on the formation of giant gas fields［J］. China Petroleum Exploration， 2015， 20（4）： 71-80.
[32] Energy IHS. Basin monitors： Ruvuma basin ［M］. Houston： IHS Inc， 2009.
[33] 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.
[34] 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.
[35] 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.
[36] Kostic S. Modeling of submarine cyclic steps： Controls on their formation， migration， and architecture［J］. Geosphere， 2011， 7（2）： 294-304.
[37] Kenyon N H， Millington J. Contrasting deep-sea depositional systems in the Bering Sea［C］//Pickering K T， Hiscott R N， Kenyon N H， et al. Atlas of deep water environments： Architectural style in turbidite systems. Dordrecht： Springer， 1995： 196-202.
[38] Morris S A， Kenyon N H， Limonov A F， et al. Downstream changes of Large-scale bedforms in turbidites around the Valencia channel mouth， north-west Mediterranean： Implications for palaeoflow reconstruction［J］. Sedimentology， 1998， 45（2）： 365-377.
[39] Cartigny M J B， Ventra D， Postma G， et al. Morphodynamics and sedimentary structures of bedforms under supercritical-flow conditions： New insights from flume experiments［J］. Sedimentology， 2014， 61（3）： 712-748.
[40] Fildani A， Hubbard S M， Covault J A， et al. Erosion at inception of deep-sea channels［J］. Marine and Petroleum Geology， 2013， 41（1）： 48-61.
[41] Hamilton P B， Strom K B， Hoyal D C J D. Hydraulic and sediment transport properties of autogenic avulsion cycles on submarine fans with supercritical distributaries［J］. Journal of Geophysical Research： Earth Surface， 2015， 120（7）： 1369-1389.
[42] Postma G， Hoyal D C， Abreu V， et al. Morphodynamics of supercritical turbidity currents in the channel-lobe transition zone［M］//Lamarche G， Mountjoy J， Bull S， et al. Submarine mass movements and their consequences. Cham： Springer， 2016： 469-478.