MODEL OF MODERN DYNAMIC DEPOSITION IN THE EAST CHINA SEA

作     者：周福根 Zhou Fugen(Marine Geological Department and Analysis & Research Center, Tongji University, Shanghai)

作者机构：Marine Geological Department and Analysis & Research Center Tongji University Shanghai 

出 版 物：《Chinese Journal of Oceanology and Limnology》 (中国海洋湖沼学报（英文版）)

年 卷 期：1989年第7卷第3期

页      面：274-282页

核心收录：

学科分类：07[理学] 

主　　题：DYNAMIC Fujian Hangzhou Taiwan eastern banks branches Jiangsu modem outflow 

摘      要：Since the last rising of sea level, two branches of the Kuroshio, the Huanghai ( Yellow Sea ) coastal current (HCC; mainly cold water mass)and the Changjiang River outflow have controlled the modem dynamic deposition in the East China Sea. There are three depositing areas on the sea-bed under the above currents: a relict sand area un der the Taiwan Warm Current and the Huanghai Warm Current at the south-eastern area, the about 60 km2 round mud bank under the Huanghai CoastalCurrent at the northernarea and the large subaqueous delta of mainly fine sand and silt under the Changjiang discharge flow in its estuary and the large narrow mud bank under the Zhejiang-Fujian Coastal Current, another round mud bank under the Changjiang discharge flow off Hangzhou Bay. The relict sand area has a coarsesand block under the Taiwan Warm Current bypassing Taiwan at the northern part of the *** two round mud banks were formed in relatively static states by an anticlockwise converging cyclonic eddy. The