从溺谷湾到三角洲：现代珠江三角洲形成演变研究辨析

吴超羽; 韦惺

doi:10.12284/hyxb2021019

从溺谷湾到三角洲：现代珠江三角洲形成演变研究辨析

doi: 10.12284/hyxb2021019

吴超羽^1,,
韦惺^{2, 3}

1.
中山大学近岸海洋科学与技术研究中心，广东广州 510275
2.
中国科学院南海海洋研究所热带海洋环境国家重点实验室，广东广州 510301
3.
南方海洋科学与工程广东省实验室（广州），广东广州 511458

基金项目: 国家自然科学基金（40331007，40176026，40406016，41890851）；“985工程”项目（105203200400006）；南方海洋科学与工程广东省实验室（广州）人才团队引进重大专项（GML2019ZD0303）。

详细信息

作者简介:
吴超羽（1944—），男，广东省开平县人，博士，从事河口海岸学研究。E-mail：eeswcy@mail.sysu.edu.cn

Kilometer 的音译。
襄大在七星岗东南约1 km。
潟湖。
辨析也适用于拟合，插值和拟合是数值分析的基础方法。一般意义上它们的区别在于：拟合是已知数据点列，从整体上接近点列；插值是已知点列并且完全经过点列。
¹⁴C委托广州地化所测定。AMS测年由波兰GADAM Centre，Silesian University of Technology测定，其余项目在中山大学地质系实验室完成。
这里的子三角洲相当于Coleman等^[91]所说末次海侵以来密西西比河冲决形成的子三角洲或三角洲叶。
中图分类号: P343.5
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出版历程
- 收稿日期: 2019-12-05
- 修回日期: 2020-03-30
- 网络出版日期: 2021-02-24
- 刊出日期: 2021-01-25

From drowned valley to delta: Discrimination and analysis on issues of the formation and evolution of the Zhujiang River Delta

Wu Chaoyu^1
,,
Wei Xing^{2, 3}

1.
Center for Coastal Ocean Science and Technology Research, Sun Yat-sen University, Guangzhou 510275, China
2.
State Key Laboratory of Tropical Oceanography, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China
3.
Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou)，Guangzhou 511458, China

摘要

摘要: 现代珠江三角洲经历了从溺谷湾到三角洲的形成演变，富有区域特色。本文提出百余年来珠江三角洲的研究可归纳为4种范式：历史描述、实地考察−学术推理、器测−学科理论和“动力−沉积−地貌”跨尺度范式，各以范例说明。基于笔者及其团队研究，对现有文献关于珠江三角洲形成演变若干重要观点提出不同意见并从多视角作必要辨析，包括：海侵盛期以来千年尺度三角洲岸线位置变化，现代珠江三角洲形成演变的模式和三角洲干流河段形成过程与机理。最后对三角洲研究中的多学科、跨尺度和时空量化做了简要讨论。
- 珠江 /
- 溺谷湾 /
- 范式 /
- 三角洲 /
- 子三角洲 /
- 沉积体 /
- 演变模式 /
- 多学科 /
- 跨尺度 /
- 时空量化
Abstract: The modern Zhujiang River Delta has experienced the formation and evolution from drowned valley to delta, which is rich in regional characteristics. The research on the Zhujiang River Delta in the past hundred years is summarized into four paradigms: historical description, field investigation-scientific reasoning, instrument applied-discipline theory and “dynamic-sedimentary-morphologic” scale-crossing paradigm. Each illustrated by superb examples and documented. Based on the research of the authors and his team, this paper puts forward several propositions concerning the formation and evolution of the Zhujiang River Delta, which are substantially different from the existing literature, and makes necessary differentiation and analysis from multiple perspectives, including the millennial-scale changes of coastline since the transgression maximum, the mode of formation and evolution of the modern Zhujiang River Delta and the development and its mechanism of the major channels of the network in the delta. Finally, the approache of interdisciplinary, scale-crossing and time-space quantification concerning delta research are briefly discussed.
- Zhujiang River /
- drowned valley /
- paradigm /
- delta /
- sub-delta /
- deposition body /
- evolution mode /
- interdiscipline /
- cross-scale /
- spatiotemporal quantification
注释:

1) Kilometer 的音译。

2) 襄大在七星岗东南约1 km。

3) 潟湖。

4) 辨析也适用于拟合，插值和拟合是数值分析的基础方法。一般意义上它们的区别在于：拟合是已知数据点列，从整体上接近点列；插值是已知点列并且完全经过点列。

5) ¹⁴C委托广州地化所测定。AMS测年由波兰GADAM Centre，Silesian University of Technology测定，其余项目在中山大学地质系实验室完成。

6) 这里的子三角洲相当于Coleman等^[91]所说末次海侵以来密西西比河冲决形成的子三角洲或三角洲叶。

HTML全文

图 1 海侵盛期珠江溺谷湾水深（钻孔具体位置见文献[63]）

Fig. 1 Water depth of the Pearl River drowned valley during the period of high transgression（see reference [63] for detailed core locations）

下载: 全尺寸图片幻灯片

图 2 海侵盛期以来珠江三角洲岸线位置变化研究比较^[55,68,81]

Fig. 2 A comparison of the evolution of shore line changes in Zhujiang River Delta since last gransgreesion maximum from different studies^[55,68,81]

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图 3 钻孔位置（a），模型计算水深（b）和联孔剖面及等时线（c）（图c修改自文献[82]）

Fig. 3 Locations of setiment cores (a), profile of water depth from PRD-LTMM (b), and bore hole cross section and isochron (c) (figure c modified according to reference [82])

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图 4 珠江（a）与密西西比河（b）子三角洲演变比较示意图（图b据文献[91]）

Fig. 4 Evolution of sub-delta of the Zhujiang River Delta (a) and sub-delta cycle of the Mississipi River Delta (figure b is based on reference [91])

下载: 全尺寸图片幻灯片

图 5 大鳌子三角洲平原部分沉积砂体组合示意图

A. 山间河流的冲积、洪积扇沉积砂体；C. 汇流和分流区沉积砂体； D1，D2.大鳌沙与大鳌岛沉积砂体；P. 边沿沉积砂体和山麓坡积物等

Fig. 5 A block diagram showing the evolution of different sand-bodies in Daao sub-delta

A. Fluvial and alluvial sand bodies; C. sand bodies in confluence and distributary area; D1, D2. sand bodies of Daao shoal and island; P. marginal and piedmont sand bodies

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图 6 全新世海侵盛期以来若干阶段每500年沉积厚度图

Fig. 6 Thickness of 500 year’s deposition since last transgression maximum

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图 7 2500 a BP 珠江河口的余流流场和西江干流河道形态

Fig. 7 The main network channels of the Zhujiang River and residual current in 2500 a BP

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表 1 若干三角洲沉积环境、过程及其子三角洲时空模式比较

Tab. 1 Comparision of the sedimentary enviroments, processes and sub-delta modes in several deltas

三角洲	沉积环境	主要动力沉积过程	沉积模式	子（亚）三角洲	参考文献
密西西比河三角洲	陆架	天然堤冲决、堆积前展、改道废弃和侵蚀破坏	主干河流冲决天然堤形成新的三角洲扇	6个子三角洲^①：时间上有明显的先后关系，空间上可部分重叠	Coleman等^[91]
长江三角洲	下切河谷喇叭湾	河口沙坝发育、堆积前展、汊道出现、北汊淤塞	河口沙坝发育、河道分汊、北汊淤塞、南汊延伸等	6个亚三角洲：时间有明显先后关系，空间上互不重叠	李从先等^[95], 陈吉余等^[94]
多瑙河三角洲	沿岸沙坝发育形成半封闭海湾	河口堆积前展、南、北中汊道先后冲决沙坝形成子三角洲扇并交替成主行水道	充填、突破和叠覆	3个子三角洲：时间上交替发生，空间上互不重叠	Panin^[105]
珠江三角洲	基岩半封闭溺谷湾，岛丘众多	地形致周边沉积、汇潮、分流沉积、峡口双向射流、浪成砂堤等各种沉积砂体复合而成	“门”控多核心“三角洲— 子三角洲—沉积体”多级沉积结构，镶嵌式充填	约10个子三角洲：时间上同时发生，空间上相邻但互不重叠	吴超羽等^[58-59], 韦惺等^[67]

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表 2 全新世以来各钻孔快速沉积时段统计

Tab. 2 The rapid deposition periods of boreholes since Holocene

孔号	平均沉积速率/(mm·a⁻¹)	≥5 mm/a 占百分比/%	≥10 mm/a 占百分比/%
PRD2	1.32	58.95	58.95
PRD3	2.13	72.86	57.32
PRD4	3.83	67.30	31.36
PRD5	3.27	65.15	42.74
PRD6	2.59	40.49	0
PRD7	5.87	67.35	67.35
PRD9	1.18	74.82	74.82
PRD10	2.54	55.44	36.76
PRD15	2.02	54.09	44.63
PRD16	1.34	53.11	42.67
PRD17	1.52	34.79	34.79
PRD18	1.32	35.42	11.49
D6	7.81	100	30.76
D02	4.67	55.55	55.55
D21	2.29	67.24	67.241
D15	6.93	65.15	65.15
ZJ3	5.87	74.54	74.54
53	2.95	52.63	52.63
D10	7.17	100	53.79
A22	4.27	69.45	40.08
均值	3.54	63.21	47.13

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表 3 珠江下游径流量（1956−1979年）

Tab. 3 Downstream runoff of the Zhujiang River (1956−1979)

河名	站名	径流量
河名	站名	年径流/（10⁸m³）	平均流量/（m³·s⁻¹）	占流域比例/%
西江	高要	2 220	7 020	73.25
北江	石角	413	1310	13.67
绥江	石狗	68.4	217	2.26
其他	−	−	−	10.82
合计		3 029.1	9 584.3	100
注：据广东省水文总站，1986。

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参考文献(114)

[1]	de Vriend H J. Mathematical modelling and large-scale coastal behavior, Part 1: physical processes[J]. Journal of Hydraulic Research, 1991, 29(6): 727−740. doi: 10.1080/00221689109498955
[2]	Cowell P J, Stive M, Niedoroda A W, et al. The coastal-tract (Part 1): a conceptual approach to aggregated modeling of low-order coastal change[J]. Journal of Coastal Research, 2004, 19(4): 812−827.
[3]	de Vriend H J. On the prediction of aggregated-scale coastal evolution[J]. Journal of Coastal Research, 2003, 19(4): 757−759.
[4]	托马斯·库恩. 科学革命的结构[M]. 金吾伦, 胡新和, 译. 北京: 北京大学出版社, 2003. Kuhn T. The Structure of Scientific Revolutions[M]. Jin Wulun, Hu Xinhe, trans. Beijing: Peking University Press, 2003.
[5]	赵焕庭. 珠江河口特征认知的发展[J]. 海洋学报, 2018, 40(7): 1−21. Zhao Huanting. Cognitive development of characteristics of the Zhujiang River Estuary[J]. Haiyang Xuebao, 2018, 40(7): 1−21.
[6]	罗家政. 顺德县志•卷三[M]. 广州: 中山大学出版社, 1853. Luo Jiazheng. Shunde County Annals (Book Three)[M]. Guangzhou: Sun Yat-sen University Press, 1853.
[7]	屈大均. 广东新语(上)[M]. 北京: 中华书局, 1984: 1−343. Qu Dajun. Guangdong New Language (1)[M]. Beijing: Zhonghua Book Company, 1984: 1−343.
[8]	柯维廉. 督办广东治河事宜处报告书: 第1期. 西江实测[M]. 广州: 广东治河事宜处, 1916: 1−124. Olivercrona G W. Report of the Engineer-in-Chief (1). River Conservancy Commission for Kwangtung (Guangdong) Province, National Government. Canton (Guangzhou)[M]. Guangzhou: The Handling of Matters at the Guangdong River, 1916: 1−124.
[9]	Heim A. Fragmentary observations in the region of Hong Kong compared with Canton[J]. Geological Survey of Kwangtung and Kwangsi, 1929, 2(1): 1−32.
[10]	陈国达. “广州三角洲”问题[J]. 科学, 1934, 18(3): 356−364. Chen Guoda. Problem of “Canton Delta”[J]. Science, 1934, 18(3): 356−364.
[11]	蔡源明. 珠江三角洲之考察纲要[J]. 方志月刊, 1934, 7(10): 1. Cai Yuanming. Survey outlines of the Pearl River Delta[J]. Local Chronicles Monthly, 1934, 7(10): 1.
[12]	罗开富. 地理系第八次野外实习[N]. 中山大学日报, 1935–12–05(2−3). Luo Kaifu. The No. 8 fieldwork of the geographical department[N]. Zhongshan University Daily, 1935–12–05(2−3).
[13]	Wu Shangshi. La dćouverte dúne ancienne plate-fome dábrasion marine[N]. Zhongshan University Daily, 1937–05–20(3−4).
[14]	Wu Shangshi. Les environs de Canton[J]. Bulletin of the Geographical Department (The Geographical Department, Sun Yat-sen University), 1937(1): 55−64.
[15]	Wu Shangshi. Topography of Guangdong[M]//Guangdong Government. Guangdong Yearbook. Shaoguan-Lianzhou: The Compiling Room of the Secretriat of Guangdong Provincial Government, 1941: 27−41.
[16]	Wu Shangshi, Zeng Zhaoxuan. Pearl river delta[J]. Lingnan Science Journal, 1947, 8(1): 105−122.
[17]	叶汇. 北江下游河道的变迁[J]. 地理学报, 1957, 24(2): 145−160. Ye Hui. Shifting river courses of the lower peikiang in Kwangtung Province[J]. Acta Geographica Sinica, 1957, 24(2): 145−160.
[18]	Ye Hui. A preliminary study on Sixianjiao−the confluence of Xijiang and Beijiang rivers[J]. Acta Scientiarum Naturalium Universitatis Sunyatseni, 1957(2): 172−183.
[19]	徐俊鸣. 珠江三角洲[M]. 广东: 广东人民出版社, 1973: 1−38. Xu Junming. Zhujiang Delta[M]. Guangzhou: Guangdong People’s Press, 1973: 1−38.
[20]	Ying Zhipu, Chen Zhiyong, Su Zelin. Formation and evolution of X-shaped channel near SixianJiao[J]. Acta Scientiarum Naturalium Universitatis Sunyatseni, 1988, 7(2): 8−14.
[21]	Pritchard D W. Salinity distribution and circulation in the Chesapeake Bay estuarine system[J]. Journal of Marine Research, 1952, 11: 106−123.
[22]	Pritchard D W. Estuarine circulation patterns[J]. Proceedings of the American Society of Civil Engineers, 1955, 81(717): 1−11.
[23]	宋长青. 地理学研究范式的思考[J]. 地理科学进展, 2016, 35(1): 1−3. Song Changqing. On paradigms of geographical research[J]. Progress in Geography, 2016, 35(1): 1−3.
[24]	李双成, 王羊, 蔡运龙. 复杂性科学视角下的地理学研究范式转型[J]. 地理学报, 2010, 65(11): 1315−1324. doi: 10.11821/xb201011001 Li Shuangcheng, Wang Yang, Cai Yunlong. The paradigm transformation of geography from the perspective of complexity sciences[J]. Acta Geographica Sinica, 2010, 65(11): 1315−1324. doi: 10.11821/xb201011001
[25]	陈寅恪. 金明馆丛稿二编[M]. 上海: 上海古籍出版社, 1980: 1-236. Chen Yinke. Second Edition of the Jingming Museum Drafts[M]. Shanghai: Shanghai Classics Publishing House, 1980: 1−236.
[26]	吴文中, 徐国璇, 李孔宏, 等. 珠江三角洲全新世沉积概述[C]//南海海岸地貌学论文集(第一集). 广州: 中国科学院南海海洋研究所, 1975: 78−87. Wu Wenzhong, Xu Guoxuan, Li Konghong, et al. Overview of holocene deposition in the Pearl River Delta[C]//South China Sea Institute of Oceanology (1). Guangzhou: South China Sea Institute of Oceanology, Chinese Academy of Sciences, 1975: 78−87.
[27]	水文地质工程地质二队. 珠江三角洲地下肥水埋藏条件与分布规律[M]//广东省地质矿产局. 广东地质科技. 广州: 广东省地质局地质科学研究, 1976. Hydrogeological Engineering Team Ⅱ. Burial condition and distribution feature of the nutritive groundwater in the Pearl River Delta[M]//Geological Bureau of Guangdong Province. Guangdong Geological Technology. Guangzhou: Geological Institute of Geological Bureau of Guangdong Province, 1976.
[28]	李平日, 黄镇国, 张仲英, 等. 珠江三角洲的形成年代[J]. 热带地理, 1982, 2(4): 21−29. Li Pingri, Huang Zhenguo, Zhang Zhongying, et al. The formation of the Pearl River Delta[J]. Tropical Geography, 1982, 2(4): 21−29.
[29]	黄镇国, 李平日, 张仲英, 等. 珠江三角洲地区晚更新世以来海平面变化及构造运动问题[J]. 热带地理, 1982, 2(1): 29−37, 63. Huang Zhenguo, Li Pingri, Zhang Zhongying, et al. Sea level change and tectonic movement in the Pearl River Delta region since late Pleistocene[J]. Tropical Geography, 1982, 2(1): 29−37, 63.
[30]	黄镇国, 李平日, 张仲英, 等. 珠江三角洲形成发育演变[M]. 广州: 科学普及出版社广州分社, 1982: 1−274. Huang Zhenguo, Li Pingri, Zhang Zhongying, et al. The Formation and Evolution of the Zhujiang River Delta[M]. Guangzhou: Popular Science Press Bureau in Guangzhou, 1982: 1−274.
[31]	李平日, 乔彭年, 郑洪汉, 等. 珠江三角洲一万年来环境演变[M]. 北京: 海洋出版社, 1991: 1−154. Li Pingri, Qiao Pengnian, Zheng Honghan, et al. The Environment Evolution of the Zhujiang Delta in the Last 10 000 Years[M]. Beijing: China Ocean Press, 1991: 1−154.
[32]	冯炎基, 李平日, 谭惠忠, 等. 珠江三角洲第四纪沉积年代学研究[J]. 热带地理, 1990, 10(3): 247−255. Feng Yanji, Li Pingri, Tan Huizhong, et al. On quaternary sedimentary chronology of the Zhujiang Delta[J]. Tropical Geography, 1990, 10(3): 247−255.
[33]	赵焕庭. 珠江河口湾伶仃洋的地形[J]. 海洋学报, 1981, 3(2): 255−274. Zhao Huanting. Bottom relief of Ling Ding Yang of the Zhujiang River Estuary[J]. Haiyang Xuebao, 1981, 3(2): 255−274.
[34]	赵焕庭. 珠江三角洲的形成和发展[J]. 海洋学报, 1982, 4(5): 595−607. Zhao Huanting. Formation and development of the Zhujiang Delta[J]. Haiyang Xuebao, 1982, 4(5): 595−607.
[35]	Yim W W S. Evidence for Quaternary environmental changes from sea-floor sediments in Hong Kong[M]//The Evolution of the East Asian Environment. Hong Kong: University of Hong Kong, 1984: 137−155.
[36]	龙云作, 霍春兰, 司桂贤, 等. 对珠江三角洲沉积特征和沉积模式的一些认识[J]. 海洋地质与第四纪地质, 1985, 5(4): 49−57. Long Yunzuo, Huo Chunlan, Si Guixian, et al. On sedimentary characteristics and model of Zhujiang River Delta[J]. Marine Geology & Quaternary Geology, 1985, 5(4): 49−57.
[37]	徐明广, 马道修, 周青伟, 等. 珠江三角洲地区第四纪海平面变化[J]. 海洋地质与第四纪地质, 1986, 6(3): 93−102. Xu Mingguang, Ma Daoxiu, Zhou Qingwei, et al. Quaternary sea-level fluctuation in Zhujiang River Delta area[J]. Marine Geology & Quaternary Geology, 1986, 6(3): 93−102.
[38]	李平日, 郑建生, 方国祥. 广州地区第四纪地质[M]. 广州: 华南理工大学出版社, 1989: 1-192. Li Pingri, Zheng Jiansheng, Fang Guoxiang. Quaternary Geology in Guangzhou Area[M]. Guangzhou: South China University of Technology Press, 1989: 1−192.
[39]	温孝胜, 赵焕庭, 张乔民, 等. 珠江河口湾沉积物岩心揭示的海陆变迁[C]//中国地理学会地貌与第四纪专业委员会. 地貌−环境−发展. 北京: 中国环境科学出版社, 1994: 54−57. Wen Xiaosheng, Zhao Huanting, Zhang Qiaomin, et al. Sea-land changes indicated from the sediment cores of the Pearl River Estuary[C]//Specialty Committee for Geomorphology and Quaternary of the Geographical Society of China. Geomorphology-Environment-Development. Beijing: China Environment Science Press, 1994: 54−57.
[40]	温孝胜, 赵焕庭, 张乔民, 等. 伶仃洋钻孔岩心的沉积特征及环境演化[J]. 海洋学报, 1997, 19(2): 121−128. Wen Xiaosheng, Zhao Huanting, Zhang Qiaomin, et al. Sedimentary characteristics and environmental evolution of drilling cores at Lingdingyang Bay[J]. Haiyang Xuebao, 1997, 19(2): 121−128.
[41]	龙云作, 霍春兰. 珠江三角洲晚第四纪沉积特征[J]. 海洋科学, 1990(4): 7−14. Long Yunzuo, Huo Chunlan. The sedimentation characteristics of Zhujiang River Delta in Late Quaternary[J]. Marine Sciences, 1990(4): 7−14.
[42]	龙云作. 珠江三角洲沉积地质学[M]. 北京: 地质出版社, 1997: 1−165. Long Yunzuo. Sediment Geology of the Pearl River Delta[M]. Beijing: Geological Publishing House, 1997: 1−165.
[43]	赵焕庭, 赵艳冰, 王文介, 等. 伶仃洋航道选线问题调查报告[C]//中国科学院南海海洋研究所. 南海海岸地貌学论文集(3). 广州: 中国科学院南海海洋研究所, 1978: 28−62. Zhao Huanting, Zhao Yanbing, Wang Wenjie, et al. Report on the problem of channel alignment in Lingdingyang[C]//South China Sea Institute of Oceanology, Chinese Academy of Sciences. Preceeding of Coastal Geomorphology of the South China Sea (3). Guangzhou: South China Sea Institute of Oceanology, Chinese Academy of Sciences, 1978: 28−62.
[44]	赵焕庭, 宋朝景, 王文介, 等. 珠江河口狮子洋水道的地形发育[M]//中国科学院南海海洋研究所. 南海海洋科学集刊第1集. 北京: 科学出版社, 1980: 17−34. Zhao Huanting, Song Chaojing, Wang Wenjie, et al. Physiographic development of Shizi Yang (Lion Channel) at the mouth of the Zhujiang (Pearl River)[M]//South China Sea Institute of Oceanology, Chinese Academy of Science. Nanhai Studia Marina Sinica (1). Beijing: Science Press, 1980: 17−34.
[45]	徐君亮, 李永兴, 陈天富. 伶仃洋的盐水入侵及盐水楔的活动规律[J]. 热带地理, 1981, 1(3): 36−44. Xu Junliang, Li Yongxing, Chen Tianfu. The patten of the invasions of saline water and the activities of the wedge in the Zhujiang Estuary[J]. Tropical Geography, 1981, 1(3): 36−44.
[46]	徐君亮, 李永兴, 蔡福祥, 等. 珠江口伶仃洋滩槽发育演变[M]. 北京: 海洋出版社, 1985: 1−182. Xu Junliang, Li Yongxing, Cai Fuxiang, et al. The Evolution of the Beach and Trough in the Lingdingyang of the Pearl River Estuary[M]. Beijing: China Ocean Press, 1985: 1−182.
[47]	董兆英, 盖广生. 《珠江口伶仃洋滩槽发育演变》简介[J]. 人民珠江, 1985(6): 50. Dong Zhaoying, Gai Guangsheng. Brief introduction of the evolution of the beach and trough in the Lingdingyang of the Pearl River Estuary[J]. Renmin Zhujiang, 1985(6): 50.
[48]	赵焕庭. 珠江河口演变[M]. 北京: 海洋出版社, 1990: 1−357. Zhao Huanting. The Evolution of the Pearl River Estuary[M]. Beijing: China Ocean Press, 1990: 1−357.
[49]	曾昭璇. 我国某些历史地貌学问题的刍议[J]. 地理研究, 1983, 2(2): 12−19. Zeng Zhaoxuan. Some questions on the historical geomorphology problem of China[J]. Geographical Research, 1983, 2(2): 12−19.
[50]	曾昭璇, 黄少敏. 珠江三角洲历史地貌学研究[M]. 广州: 广东高等教育出版社, 1987: 1−201. Zeng Zhaoxuan, Huang Shaomin. Historical Geomorphology of the Pearl River Delta[M]. Guangzhou: Guangdong Higher Education Press, 1987: 1−201.
[51]	曾昭璇. 珠江三角洲地貌发育[M]. 广州: 暨南大学出版社, 2012: 1−172. Zeng Zhaoxuan. Geomorphological Development of the Pearl River Delta[M]. Guangzhou: Jinan University Press, 2012: 1−172.
[52]	戴勇, 王平, 金文华. 探究河口巡研海岸: 陈吉余传[M]. 上海: 上海交通大学出版社, 2015: 1−251. Dai Yong, Wang Ping, Jin Wenhua. Biography of Chen Jiyu[M]. Shanghai: Shanghai Jiao Tong University Press, 2015: 1−251.
[53]	柴立和. 多尺度科学的研究进展[J]. 化学进展, 2005, 17(2): 186−191. doi: 10.3321/j.issn:1005-281X.2005.02.002 Chai Lihe. Recent progress of multiscale science[J]. Progress in Chemistry, 2005, 17(2): 186−191. doi: 10.3321/j.issn:1005-281X.2005.02.002
[54]	Dastgheib A, Roelvink J A, Wang Z B. Long-term process-based morphological modeling of the Marsdiep tidal basin[J]. Marine Geology, 2008, 256(1/4): 90−100.
[55]	Wu Chaoyu, Bao Yun, Ren Jie, et al. A study on the Pearl River Delta in the last 6000 years: A long-term modeling approach[C]//International Conference on Tidal Dynamics and Environment (TIDALITE 2002). Nanjing: Nanjing University Press, 2002.
[56]	任杰. 末次海进盛期以来珠江三角洲演变的长周期动力地形模型及应用[D]. 广州: 中山大学, 2003. Ren Jie. The long-term dynamic terrain model and its application in the evolution of the Pearl River Delta since the Last Great Ocean Expansion[D]. Guangzhou: Sun Yat-sen University, 2003.
[57]	谭艳晖. 珠江三角洲沉积模式研究—应用长周期数值模型的实验[D]. 广州: 中山大学, 2005. Tan Yanhui. A study on the deposition modes of the Pearl River Delta: An experimentation approach by long-term numerical model[D]. Guangzhou: Sun Yat-sen University, 2005.
[58]	吴超羽, 包芸, 任杰, 等. 珠江三角洲及河网形成演变的数值模拟和地貌动力学分析: 距今6 000−2 500 a[J]. 海洋学报, 2006, 28(4): 64−80. Wu Chaoyu, Bao Yun, Ren Jie, et al. A numerical simulation and mophodynamic analysis on the evolution of the Zhujiang River Delta in China: 6 000−2 500 a BP[J]. Haiyang Xuebao, 2006, 28(4): 64−80.
[59]	Wu C Y, Ren, J, Bao Y, et al. A long-term hybrid morphological modeling study on the evolution of the Pearl River Delta network system and estuarine bays since 6000 aBP[C]//Harff J, Hay W W, Tetzlaff D F. Coastline Changes: Interrelation of Climate and Geological Processes. Geological Society of America Special Papers, 2007, 426: 199−214.
[60]	吴超羽, 任杰, 包芸, 等. 珠江河口“门”的地貌动力学初探[J]. 地理学报, 2006, 61(5): 537−548. doi: 10.3321/j.issn:0375-5444.2006.05.010 Wu Chaoyu, Ren Jie, Bao Yun, et al. A preliminary study on the morphodynamic evolution of the “gate” of the Pearl River Delta, China[J]. Acta Geographica Sinica, 2006, 61(5): 537−548. doi: 10.3321/j.issn:0375-5444.2006.05.010
[61]	任杰, 吴超羽, 贾良文. 长周期动力地形模型中代表输入条件[J]. 水科学进展, 2006, 17(2): 278−282. doi: 10.3321/j.issn:1001-6791.2006.02.021 Ren Jie, Wu Chaoyu, Jia Liangwen. Representative conditions of the long-term morphodynamic model[J]. Advances in Water Science, 2006, 17(2): 278−282. doi: 10.3321/j.issn:1001-6791.2006.02.021
[62]	何志刚, 吴超羽, 莫文渊, 等. 冰后期珠江三角洲沉积物通量的初步研究[J]. 海洋学报, 2006, 28(6): 72−77. He Zhigang, Wu Chaoyu, Mo Wenyuan, et al. A preliminary study on sediment flux in the Zhujiang River Delta during the postglacial period[J]. Haiyang Xuebao, 2006, 28(6): 72−77.
[63]	何志刚. 珠江三角洲大鳌平原形成与古磨刀门动力演变的互动机制研究[D]. 广州: 中山大学, 2006. He Zhigang. A study of the mechanism of the interaction between the formation of Da’ao plain and dynamic processes of paleo-modao gate in Pearl River Delta[D]. Guangzhou: Sun Yat-sen University, 2006.
[64]	何志刚, 莫文渊, 刘春莲, 等. 从沉积速率和沉积物粒度看冰后期海侵以来珠江三角洲西江大鳌沙的形成[J]. 古地理学报, 2007, 9(3): 331−336. doi: 10.3969/j.issn.1671-1505.2007.03.011 He Zhigang, Mo Wenyuan, Liu Chunlian, et al. Formation of Xijiang Da’aosha in Pearl River Delta during the postglacial period from a perspective of sedimentation rates and sediment grain size[J]. Journal of Palaeogeography, 2007, 9(3): 331−336. doi: 10.3969/j.issn.1671-1505.2007.03.011
[65]	任杰, 吴超羽, 包芸. 长周期动力形态模型中地形演变方法探讨[J]. 海洋学报, 2007, 29(1): 76−80. Ren Jie, Wu Chaoyu, Bao Yun. Approaches to morphological evolution in long-term morphodynamic model[J]. Haiyang Xuebao, 2007, 29(1): 76−80.
[66]	吴超羽, 何志刚, 任杰, 等. 珠江三角洲中部子平原形成演变机理研究—以大鳌平原为例[J]. 第四纪研究, 2007, 27(5): 814−827. doi: 10.3321/j.issn:1001-7410.2007.05.023 Wu Chaoyu, He Zhigang, Ren Jie, et al. Physical study on the evolution of the sub-deltaic plains in the mid Zhujiang River Delta: A case study of da’ao sub-delta[J]. Quaternary Sciences, 2007, 27(5): 814−827. doi: 10.3321/j.issn:1001-7410.2007.05.023
[67]	韦惺, 吴超羽, 任杰, 等. 6 ka以来广州溺谷湾形成演变的数值模拟和地貌动力学分析[J]. 中国科学 D辑: 地球科学, 2008, 38(11): 1384−1395. Wei Xing, Wu Chaoyu, Ren Jie, et al. A numerical simulation and mophodynamic analysis on the evolution of the drowned valley bay of Guangzhou since 6 ka[J]. Science China Earth Sciences, 2008, 38(11): 1384−1395.
[68]	Wei Xing, Wu Chaoyu. Long-term process-based morphodynamic modeling of the Pearl River Delta[J]. Ocean Dynamics, 2014, 64(12): 1753−1765. doi: 10.1007/s10236-014-0785-7
[69]	张文彦. 波浪主导型海岸长周期形态动力演变的多尺度建模研究[D]. 广州: 中山大学, 2010. Zhang Wenyan. A multi-scale morphodynamic modeling methodology for long-term evolution of wave-dominated coasts[D]. Guangzhou: Sun Yat-sen University, 2010.
[70]	Zhang Wenyan, Harff J, Schneider R, et al. Development of a modelling methodology for simulation of long-term morphological evolution of the southern Baltic coast[J]. Ocean Dynamics, 2010, 60(5): 1085−1114. doi: 10.1007/s10236-010-0311-5
[71]	刘斌. 珠江磨刀门河口十年尺度地形演变数值模拟[D]. 广州: 中山大学, 2005. Liu Bin. Numerical simulation of the ten-year scale topographic evolvement of “modao” Gate of Pearl River[D]. Guangzhou: Sun Yat-sen University, 2005.
[72]	邱立国. 磨刀门海区长时间尺度地形演变数值模拟与地貌动力分析—基于强人类活动影响下[D]. 广州: 中山大学, 2006. Qiu Liguo. Numerical simulation of the long-term topographic evolution for the Modaomen coastal area of the Pearl River and morphodynamic analysis: Under the influence of severe human activities[D]. Guangzhou: Sun Yat-sen University, 2006.
[73]	刘斌, 吕海滨, 吴超羽, 等. 磨刀门河口在20世纪60至70年代的演变模拟与动力地貌过程分析[J]. 海洋学报, 2014, 36(2): 75−80. Liu Bin, Lü Haibin, Wu Chaoyu, et al. The evolution simulation and dynamic geomorphic process analysis of Modaomen Estuary from the 1960s to the 1970s[J]. Haiyang Xuebao, 2014, 36(2): 75−80.
[74]	许炜铭. 十到百年尺度人类活动作用下珠江河口演变的案例研究[D]. 广州: 中山大学, 2010. Xu Weiming. Case studies of decade-to-century-scale evolution of Pearl River estuary influenced by human activities[D]. Guangzhou: Sun Yat-sen University, 2010.
[75]	邱立国, 韦惺, 莫文渊, 等. 十到百年尺度动力形态模型在珠江磨刀门河口的应用[J]. 海洋学报, 2012, 34(4): 135−146. Qiu Liguo, Wei Xing, Mo Wenyuan, et al. A long-term numerical model of mophodynamic evolution and its application to Modaomen Estuary[J]. Haiyang Xuebao, 2012, 34(4): 135−146.
[76]	刘欢. 珠江河口地形致高能耗区的消能特点和机理研究[D]. 广州: 中山大学, 2009. Liu Huan. Characteristic and mechanism of energy dissipation in topography-induced hotspots in the Pearl River Estuary[D]. Guangzhou: Sun Yat-sen University, 2009.
[77]	Liu Huan, Wu Chaoyu, Xu Weiming, et al. Contrasts between estuarine and river systems in near-bed turbulent flows in the Zhujiang (Pearl River) Estuary, China[J]. Estuarine, Coastal and Shelf Science, 2009, 83(4): 591−601. doi: 10.1016/j.ecss.2009.05.005
[78]	刘欢, 尹小玲, 吴超羽, 等. 珠江河口潮流底边界层的湍流特征量研究[J]. 水动力学研究与进展, 2009, 24(2): 133−140. Liu Huan, Yin Xiaoling, Wu Chaoyu, et al. Turbulence feature research within bottom boundary layer induced by tide in the Pearl River Estuary[J]. Journal of Hydrodynamics, 2009, 24(2): 133−140.
[79]	倪培桐. 地形致动力场对珠江河口能量耗散及其作用机制[D]. 广州: 中山大学, 2010. Ni Peitong. Characteristic and mechanism of energy dissipation made by dynamic structure induced by topography in the Pearl River Estuary[D]. Guangzhou: Sun Yat-sen University, 2010.
[80]	倪培桐, 吴超羽, 刘欢. “门”地貌单元的能量耗散和过程机制[J]. 热带海洋学报, 2012, 31(2): 34−40. doi: 10.3969/j.issn.1009-5470.2012.02.005 Ni Peitong, Wu Chaoyu, Liu Huan. Energy dissipation and its mechanism induced by “gate” topography[J]. Journal of Tropical Oceanography, 2012, 31(2): 34−40. doi: 10.3969/j.issn.1009-5470.2012.02.005
[81]	Zong Yongqiang, Huang G, Switzer A D, et al. An evolutionary model for the Holocene formation of the Pearl River Delta, China[J]. The Holocene, 2009, 19(1): 129−142. doi: 10.1177/0959683608098957
[82]	Wei Xing, Wu Chaoyu. Holocene delta evolution and sequence stratigraphy of the Pearl River Delta in South China. Science China Earth Sciences, 2011, 54: 1523–1541.
[83]	Wu Chaoyu, Zhou Di. Long-term morpho-dynamics in special type of estuary[J]. Science in China Series B: Chemistry, 2001, 44(1): 112−125.
[84]	Wu Chaoyu, Wei Xing, Ren Jie, et al. Morphodynamics of the rock-bound outlets of the Pearl River Estuary, South China−A preliminary study[J]. Journal of Marine Systems, 2010, 80(S1): S17−S27.
[85]	钱宁, 万兆惠. 泥沙运动力学[M]. 北京: 科学出版社, 2003: 1−687. Qian Ning, Wan Zhaohui. Mechanics of Sediment Transport[M]. Beijing: Science Press, 2003: 1−687.
[86]	吴超羽. 珠江三角洲千年尺度演变的动态平衡及其唯象判据探讨[J]. 海洋学报, 2018, 40(7): 22−37. Wu Chaoyu. A preliminary study on the phenomenological relation between morphodynamic equilibrium and geomorphic information entropy in the evolution of the Zhujiang River Delta[J]. Haiyang Xuebao, 2018, 40(7): 22−37.
[87]	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.
[88]	Galloway W E. Process framework for describing the morphologic and stratigraphic evolution of deltaic depositional systems. In Deltas, Models for Exploration, Broussard ML (ed.) [M]. Houston: Houston Geological Society, 1975: 87–98.
[89]	Fisk H N. Geological investigation of the alluvial valley of the Lower Mississippi River[R]. Washington, DC: U. S. Army Corps of Engineers, 1944: 78.
[90]	Fisk H N. Mississippi River valley geology relation to river regime[J]. Transactions of the American Association of Civil Engineers, 1952, 117: 667−689.
[91]	Coleman J M, Roberts H H, Stone G W. Mississippi River Delta: an overview[J]. Journal of Coastal Research, 1998, 14(3): 698−716.
[92]	陈吉余. 长江三角洲江口段的地形发育[J]. 地理学报, 1957, 23(3): 241−253. Chen Jiyu. Notes on the development of the Yangtze estuary[J]. Acta Geographica Sinica, 1957, 23(3): 241−253.
[93]	陈吉余, 虞志英, 恽才兴. 长江三角洲的地貌发育[J]. 地理学报, 1959, 26(3): 201−220. Chen Jiyu, Yu Zhiying, Yun Caixing. The geomorphologic development of the Yangtze River Delta[J]. Acta Geographica Sinica, 1959, 26(3): 201−220.
[94]	陈吉余, 恽才兴, 徐海根, 等. 两千年来长江河口发育的模式[J]. 海洋学报, 1979, 1(1): 103−111. Chen Jiyu, Yun Caixing, Xu Haigen, et al. The developmental model of the Changjiang River Estuary during last 2000 years[J]. Haiyang Xuebao, 1979, 1(1): 103−111.
[95]	李从先, 郭蓄民, 许世远, 等. 全新世长江三角洲地区砂体的特征和分布[J]. 海洋学报, 1979, 1(2): 252−268. Li Congxian, Guo Xumin, Xu Shiyuan, et al. The characteristics and distribution of Holocene sand bodies in Changjiang River Delta area[J]. Haiyang Xuebao, 1979, 1(2): 252−268.
[96]	Hori K, Tanabe S, Saito Y, et al. Delta initiation and Holocene sea-level change: example from the Song Hong (Red River) delta, Vietnam[J]. Sedimentary Geology, 2004, 164(3/4): 237−249.
[97]	宋兵. 全新世长江三角洲初始发育及其主要影响因素探讨[D]. 上海: 华东师范大学, 2014: 1-129. Song Bing. Initiation of Changjiang (Yangtze) Delta and its primary factors during the Holocene[D]. Shanghai: East China Normal University, 2014: 1−129.
[98]	曾昭璇, 黄少敏. 西江下游中山冲缺三角洲地貌发育的历史分析[J]. 华南师范学院学报(自然科学版), 1980(2): 83−96. Zeng Zhaoxuan, Huang Shaomin. Historical analysis of the geomorphological development of the Zhongshan Gap-Cut Delta in the lower reaches of the Xijiang[J]. Journal of South China Normal University (Natural Science Edition), 1980(2): 83−96.
[99]	曾昭璇. 各个三角洲地貌发育概况[J]. 热带地貌, 1981(2): 9−33. Zeng Zhaoxuan. A summary of the development of deltas geomorphology[J]. Tropical Geomorphology, 1981(2): 9−33.
[100]	李春初. 全新世河口三角洲形成发展的若干问题—以珠江河口三角洲为例[J]. 中山大学学报, 1987(3): 9−16. Li Chunchu. Some problems on the development of Zhujiang (Pearl River) Estuary and Delta during the Holocene Epoch[J]. Acta Scientiarum Naturalium Universitatis Sunyatseni, 1987(3): 9−16.
[101]	张虎男. 断块型三角洲[J]. 地理学报, 1980, 35(1): 58−67. doi: 10.3321/j.issn:0375-5444.1980.01.006 Zhang Hu’nan. The fault delta[J]. Acta Geographica Sinica, 1980, 35(1): 58−67. doi: 10.3321/j.issn:0375-5444.1980.01.006
[102]	黄玉昆, 夏法, 黄导繁, 等. 南海北部沿岸全新世海面变动与近代地壳运动[J]. 海洋学报, 1982, 4(6): 713−723. Huang Yukun, Xia Fa, Huang Daofan, et al. Holocene sea level fluctuation and crustal movement along the northern coast of the South China Sea[J]. Haiyang Xuebao, 1982, 4(6): 713−723.
[103]	陈伟光, 赵红梅, 常郁, 等. 珠江三角洲晚第四纪垂直构造运动速率[J]. 地震地质, 2001, 23(4): 527−536. doi: 10.3969/j.issn.0253-4967.2001.04.006 Chen Weiguang, Zhao Hongmei, Chang Yu, et al. The rate of late Quaternary vertical motion of the Zhujiang Delta[J]. Seismology and Geology, 2001, 23(4): 527−536. doi: 10.3969/j.issn.0253-4967.2001.04.006
[104]	姚衍桃, 詹文欢, 刘再峰, 等. 珠江三角洲的新构造运动及其与三角洲演化的关系[J]. 华南地震, 2008, 28(1): 29−40. doi: 10.3969/j.issn.1001-8662.2008.01.004 Yao Yantao, Zhan Wenhuan, Liu Zaifeng, et al. Neotectonics of the Pear River Delta and its relationship with the deltaic evolution[J]. South China Journal of Seismology, 2008, 28(1): 29−40. doi: 10.3969/j.issn.1001-8662.2008.01.004
[105]	Panin N. The danube delta. Geomorphology and Holocene evolution: a synthesis[J]. Géomorphologie: Relief, Processus, Environnement, 2003, 9(4): 247−262.
[106]	莫文渊, 韦惺, 吴超羽. 全新世以来珠江三角洲海鸥沙形成过程的地貌动力学分析[J]. 热带海洋学报, 2019, 38(3): 68−78. Mo Wenyuan, Wei Xing, Wu Chaoyu. Morphodynamic analysis of Haiou sandbody evolution in Pearl River Delta since Holocene[J]. Journal of Tropical Oceanography, 2019, 38(3): 68−78.
[107]	郑卓, 汤永杰, 郑艳伟, 等. 西江—北江及珠江三角洲汇流区全新世泥炭腐木层时空分布与环境变化[J]. 热带地理, 2016, 36(3): 313−325. Zheng Zhuo, Tang Yongjie, Zheng Yanwei, et al. Environmental changes inferred from spatial-temporal distribution of Holocene Buried Peat layers in lower reaches of the Xijiang and Beijiang and the River confluence of Pearl River Delta[J]. Tropical Geography, 2016, 36(3): 313−325.
[108]	黄康有, 何嘉卉, 宗永强, 等. 珠江三角洲三水盆地早全新世以来孢粉分析与古环境重建[J]. 热带地理, 2016, 36(3): 364−373. Huang Kangyou, He Jiahui, Zong Yongqiang, et al. Holocene paleoenvironment reconstruction based on Pollen data in the Sanshui Basin, Northern Pearl River Delta[J]. Tropical Geography, 2016, 36(3): 364−373.
[109]	余东华. 6 000−2 500 a BP珠江三角洲西江主干河道发育演变及其数值模拟研究[D]. 广州: 中山大学, 2010: 1−133. Yu Donghua. A numerical simulation and mophodynamic analysis on the evolution of the Xijiang main channel since 6 000−2 500 a BP[D]. Guangzhou: Sun Yat-sen University, 2010: 1−133.
[110]	韦惺. 广州溺谷湾形成演变的数值模拟和地貌动力学分析[D]. 广州: 中山大学, 2007. Wei Xing. A numerical simulation and mophodynamic analysis on the evolution of the drowned valley bay of Guangzhou[D]. Guangzhou: Sun Yat-sen University, 2007.
[111]	曾昭璇. 思贤滘—历史地形学研究[J]. 人民珠江, 1982(1): 8−13, 17. Zeng Zhaoxuan. Historical topography study on the Sixianjiao[J]. Renmin Zhujiang, 1982(1): 8−13, 17.
[112]	彭加勒. 科学与方法[M]. 李醒民, 译. 北京: 商务印书馆, 2006. Poincaré J H. Science and Method[M]. Li Xingmin, trans. Beijing: The Commercial Press, 2006.
[113]	普朗克. 世界物理图景的统一性[M]. 莫斯科: 莫斯科出版社, 1966: 1−183. Planck M. Unity of the Physical Landscape of the World[M]. Moscow: Moscow Press, 1966: 1−183.
[114]	Cross T A. High-resolution stratigraphic correlation from the perspectives of base-level cycles and sediment accommodation[C]//Dolson J. Unconformity Related Hydrocarbon Exploration and Accumulation in Elastic and Carbonate Settings. Colorado: Rocky Mountain Association of Geologists, 1991: 28−41.