[1] 黄镇国,李平日,张仲英等.珠江三角洲形成发育演变[M].广州:科学普及出版社分社,1982.274[Huang Z,Li P,Zhang Z,et al. Formation,development and evolution of Pear River Delta[M].Guangzhou:Science Populariztion Press,1982.274]
[2] 黄镇国,李伟强,赖冠文等.珠江三角洲海平面上升对堤围防御能力的影响[J].地理学报,1999,54(6): 518~535[Huang Z,Li W,Lai G,et al.The influence of sea level rising on the embankments in the Zhujiang Delta[J]. Acta Geographica Sinica,1999,54(6):518~535]
[3] 李春初,王鸿寿,杨干然等.西江下游(梧州至磨刀门)河床床沙特征及其反映的沿程泥沙运动规律,海岸河口区动力、地貌、沉积过程论文集[M].北京:科学出版社,1985,111~119[Li C, Wang H,Yang G,et al. River bed sediment characteristics and its transporation rule.Dynamics,Geomorphology and Sedimentation in Coast and Estuary[M].Beijing:Science Press,1985.111~119]
[4] 乔彭年.珠江三角洲河网发育的成因分析[J].人民珠江,1981,(2): 32 [Qiao P.Analysis of formation cause of a river net in Zhujiang Delta[J].Renmin Zhujiang,1981,(2):32]
[5] 乔彭年.珠江三角洲西江干流河床演变的近代过程[J].地理科学,1983,3(2): 141~150[Qiao P.Neoteric process of Xijiang trunk channel evolution in the Zhujiang Delta[J].Geographical Science,1983,3(3):141~150]
[6] 李平日,乔彭年.珠江三角洲六千年来的发育模式[J].泥沙研究,1982,(3): 33~42[Li P, Qiao P.Developmental mode of the Zhujiang Delta since 6000 years[J].Sediment Research,1982,(3):33~42]
[7] 彭苏萍.复合型三角洲平原上网状河的基本特征[J].科学通报,1989,34(17): 1326~132[Neng S.The basic characterstics of the asnastomosing river in multipe deltas[J].Science Bulletin,34(17):1 326~1 328]
[8] 张周良,王芳华.广东三水盆地第四纪网状河沉积特征[J].沉积学报,1997,15(4): 58~63[Zhang Z,Wang F.Sedimentary characteristics of a quaternary anastomosing river in Sanshui Basin,Guangdong Province[J].Acta Sedimentologica Sinica,1997,15(4):58~63]
[9] Smith D G,Putnam P E. Anastomosed river deposits: modern and ancient examples in Alberta, Canada[J]. Canadian Journal of Earth Sciences,1980, 17: 1 396~1 406
[10] Smith D G, Smith N D. Sedimentation in anastomosed river systems: examples from alluvial vallays near Banff, Alberta[J]. Journal of Sedimentary Petrology, 1980,50: 157~164
[11] 王随继,任明达.根据河道形态和沉积物特征的河流新分类[J].沉积学报, 1999, 17(2): 240~246[Wang S,Ren M.A new classification of fluvial rivers according to channel planforms and sediment characteristicas[J].Acta Sedimentologica Sinica,1999,17(2):240~246]
[12] Smith D G. Anastomosing river deposits, sedimentation rates and basin subsidence, Magdalena River, northwestern Columbia, South America[J]. Sediment. Geol., 1986,46: 177~196
[13] 王随继,尹寿鹏.网状河流和分汊河流的河型归属讨论[J].地学前缘,2000, 7(s): 79~86[Wang S,Yin S. Discussion on channel pattens of anastomosing and anabranched rivers[J].Earth Science Frontiers,2000,7(s):79~86]
[14] Smith N D, Cross T A, Dufficy J P, Clough S R. Anatomy of an avulsion[J]. Sedimentology,1989, 36: 1~23
[15] McCarthy T S, Ellery W N, Stanistreet I G. Avulsion mechanisms on the Okavango fan, Botswana: the control of a fluvial system by vegetation[J]. Sedimentology, 1992,39: 779~795
[16] 王随继.网状河流的河性、区域特点及多河道形成机理[D].北京:清华大学.2000[Wang S.General characteristics,local tratis and multiple-channel formation mechanism of anastomosing river[D].Beijing:Tsinghua University,2000]