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《Marine Science Bulletin》 1983-03
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QIAN LIPING,LI YULIANG,ZHU ZIMIN and CAI WEIQING(Institute of Marine Geology. Tongji University)  
When the postglacial transgression of the Holocene Epoch was at its period of full bloom 7,500 years ago,the Changjiang River mouth receded inland,thus forming an estuary in the shape of a horn with Zhenjiang and Yangzhou located at its tips.This made it impossible for the silt of the Changjiang River to reach and affect the coastal areas of Zhejiang and Fujian.During this period,the Zhoushan Archipelago suffered serious erosion,which developed a wide sea-eroded landform.Later,a gradual decrease in the uplift rate of sea level led to a rapid growth of the current Changjiang River delta and gradual southward shift of the Changjiang River mouth.The littoral current carried a large amount of silt southward,and the erosion of the coastal zone of the Zhoushan area came to a stop.A great deal of marine ooze lay directly on top of the sea-eroded landform and the marine sand-gravel bed,thus bringing about a sudden change in sedimentary facies.With the constant supply of the silt from the Changjinag River and the continuous uplifting of this area,a large area of mud beach was formed,and a coastal zone of the erosion-accumulation type widely developed.This gives rise to the possibility of the islands being joined up by mudbank.
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1 Cai Aizhi(Institute of Oceanology, Academia Sinica, Qingdao);DIFFUSION OF SEDIMENTS OF THE CHANGJIANG RIVER DISCHARGING INTO THE SEA[J];Acta Oceanologica Sinica;1982-01
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1 Shi Liren, Wei Te, Shen Huishu;The Diffusion of Seaward Sediments from Yangtze River and the Source of Depositing Sediments in the North Branch[J];;1985-02
2 Sun Ying and Huang Wensheng (Estuarine and Harbour Research Division of the Hangzhou University);The Siltation Process and Silt Sources of the Zhejiang Coast[J];Donghai Marine Science;1984-04
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9 PANG Chongguang WANG Fan Institute of Oceanology, The Chinese Academy of Sciences, Qingdao 266071;The Distributing Features and Temporal Variability of Suspended Matter Concentration in the East China Sea[J];Studia Marina Sinica;2004-00
10 Zhou Kaisheng1, Meng Yi2, Liu Cangzi2, Hong Xueqing3 (1. Department of Foodstuff and Bioengineering, Bengbu College, Bengbu 233030, China; 2. State Key Laboratory of Eastuarine and Coastal Research, Institue of Eastuarine and Coastal Research, East China Normal Uniersity, Shanghai 200062, China; 3. Department of Geography, East China Normal University, Shanghai 200062, China);Analysis of the source of tidal sandy sediments in the north branch of Changjiang River esturary[J];Journal of Hainan Normal University(Natural Science);2007-03
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1 NING CHIEN, HAN-SIANG SIE, CHIH-TEH CHOW QUAN-PIN LEE (Institute of Hydrotechnical Research) (Institute of Hydraulic Research, Chekiang Province);THE FLUVIAL PROCESSES OF THE BIG SAND BAR INSIDE THE CHIEN TANG CHIANG ESTUARY[J];Acta Geographica Sinica;1964-02
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7 CAI WEIZHANG CHEN GENXIN(Second Institute of Oceanography, NBO)DING JINREN(Zhejiang Provincial Institute of Estuarine and Coastal Engineering Research);A DISCUSSION OF THE FEATURES OF THE TIDE AND TIDAL CURRENT IN THE XIANGSHAN HARBOUR AND THEIR CAUSE OF FORMATION[J];Marine Science Bulletin;1985-03
8 Wang Zongtao (Hangzhou University);THE CHANGES OF SEA-LEVEL IN HOLOCENE ON THE COAST OF ZHEJIANG[J];;1982-02
9 Wang Pinxian Ye Guoliang(Tongji University) {The Sixth Mineral Exploring Team of Zhejiang Province)andBian Yunhua (Tongji University);MICROPALEONTOLOGICAL EVIDENCE FOR THE HISTORY OF WEST LAKE, HANGZHOU, ZHEJIANG PROVINCE, CHINA[J];Oceanologia Et Limnologia Sinica;1979-04
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10 ZHANG Zhen-ke,XIE Li,CONG Ning,LI Ying,WANG Xiu-ling,HE Hua-chun(School of Geographic and Oceanographic Sciences,MOE Key Lab. of Coast &Island Development,Nanjing University,Nanjing 210093,China);Recent morphological changes of tidal flat at Yuantuojiao Point,estuary of the north branch of the Yangtze River[J];Geographical Research;2010-05
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