[1] Crossland C J, Kremer H H, Lindeboom H J, et al.Coastal Fluxes in the Anthropocene.Berlin: Springer,2005.1~37.
[2] Allen J R L.Morphodynamics of Holocene salt marshes: A review sketch from the Atlantic and Southern North Sea coasts of Europe.Quaternary Science Reviews, 2000,(19):1155~1231.
[3] Pethick J. Estuarine and tidal wetland restoration in the United Kingdom: Policy versus practice. Restoration Ecology,2002, (10): 431~437.
[4] King S E, Lester J N. Pollution Economics:The value of saltmarshes as a sea defence.Marine Pollution Bulletin, 1995,(30):180~189.
[5] 时钟,陈吉余,虞志英.中国淤泥质潮滩沉积研究的进展.地球科学进展, 1996,11(6):555~562.
[6] 任美锷.中国淤泥质潮滩沉积研究的若干问题.热带海洋,1985,(4):6~14.
[7] 朱大奎,柯贤坤,高抒.江苏海岸潮滩沉积的研究.黄渤海海洋,1986,4(3):19~27.
[8] 李成治,李本川.苏北沿海暗沙成因的研究.海洋与湖沼,1981,12(4):321~331.
[9] Ying Wang.The mudflat coast of China.Canada Journal of Fisheries and Aquatic Sciences, 1983, 40(1):160~171.
[10] 张忍顺. 江苏省淤泥质潮滩的潮流特征及悬移质沉积过程.海洋与湖沼, 1986, 17 (3) : 235~ 245.
[11] 李从先,杨学君,庄振业,等.淤泥质海岸潮间浅滩的形成和演变.山东海洋学院学报,1965,(2):21~31.
[12] 李从先,赵娟. 苏北弶港辐射沙洲研究的进展和争论.海洋科学,1995,(4):57~59.
[13] 任美锷,张忍顺,杨巨海,等.风暴潮对淤泥质海岸的影响.海洋地质与第四纪地质,1983,3(4):1~24.
[14] 任美锷,张忍顺,杨巨海,等.江苏王港地区淤泥质潮滩的沉积作用.海洋通报,1984,3(1):40~50.
[15] 许世远,邵虚生,洪雪晴,等.杭州湾北部沿岸的风暴沉积.中国科学(B辑),1984,(12):1136~1148.
[16] 逢自安.浙江港湾淤泥质海岸剖面若干特性.海洋科学,1980,12(2):9~14.
[17] 王宝灿,虞志英,刘苍字,等.海州湾岸滩演变和泥沙流向.海洋学报,1980,2(1):23~84.
[18] 黄海军,李成治.南黄海海底辐射沙洲的现代变迁研究.海洋与湖沼,1998,29(6):640~645.
[19] Wang Yaping,Gao Shu, Jia Jianjun.High-resolution data collection for analysis of sediment dynamic processes associated with combined current-wave action over intertidal flats.Chinese Science Bulletin,2006, 51(7):866~877.
[20] Li Z H, Gao S, Chen S L, et al.Grain size distribution patterns of suspended sediment in response to hydrodynamics on the Dafeng intertidal flats, Jiangsu, China. Acta Oceanologica Sinica, 2006,25(6):63~77.
[21] 杨世伦.长江三角洲潮滩季节性冲淤循环的多因子分析.地理学报,1997,52(2):123~130.
[22] 付桂,李九发,应铭,等.长江河口南汇嘴潮滩近期演变分析.海洋通报,2007,26(2):105~112.
[23] 黄海军,李凡,庞家珍,等.黄河三角洲与渤、黄海陆海相互作用研究.北京:科学出版社,2005.1~313.
[24] 王颖.黄海陆架辐射沙脊群.北京:中国环境科学出版社,2002.1~433.
[25] Yang S L, Belkin I M, Belkina A I, et al. Delta response to decline in sediment supply from the Yangtze River: Evidence of the recent four decades and expectations for the next half century.Estuarine, Coastal and Shelf Science, 2003, (57):589~599.
[26] 李伯昌.1984年以来长江口北支演变分析.水利水运工程学报,2006,(3):9~17.
[27] 陈沈良,谷国传,刘勇胜.长江口北支涌潮的形成条件及其初生地探讨.水利学报,2003,(11):30~37.
[28] 杨欧,刘苍字.长江口北支沉积物粒径趋势及泥沙来源研究.水利学报,2002,(2):79~84.
[29] 张振克,李彦明,孟红明,等.江苏圆陀角附近潮滩沉积岩芯粒度变化及其环境意义.第四纪研究,2008,28(4): 690~694.
[30] 夏东兴,王文海,武桂秋,等.中国海岸侵蚀述要.地理学报,1993,48(5):468~476.
[31] 季子修.中国海岸侵蚀特点及侵蚀加剧原因分析.自然灾害学报,1996,5(2):65~75.
[32] Hansom J D. Coastal sensitivity to environmental change: A view from the beach. Catena, 2001, 42: 291~305.
[33] 季子修,蒋自巽,朱季文,等.海平面上升对长江三角洲附近沿海潮滩和湿地的影响.海洋与湖沼, 1994, 25(6): 582~590.
[34] 杨作升,陈晓辉.百年来长江口泥质区高分辨率沉积粒度变化及影响因素探讨.第四纪研究, 2007, 27(5): 690 ~699.
[35] Allen J R L. Evolution of salt-marsh cliffs in muddy and sandy systems:a qualitative comparison of British west coast estuaries. Earth Surface Processes and Landforms, 1989,(14): 85~92.
[36] 高抒, Collins M.英格兰南部克赖斯特切奇港在堆积环境中盐沼湿地边缘陡坎的成因.见:许东禹.第三十届国际地质大会文集·海洋地质学古海洋学.北京:地质出版社, 1999.74~85.
[37] 张忍顺,陆丽云,王艳红.江苏海岸侵蚀过程及其趋势.地理研究,2002,21(4):469~478.
[38] 杨桂山,施雅风,季子修.江苏淤泥质潮滩对海平面变化的形态响应.地理学报,2002,57(1):76~84.
[39] 陈宏友.苏北南通海涂近期冲淤动态及其开发.海洋科学,1990,(2):28~34.
|