摘要
通过对现场水文和地貌调查资料的分析,得出山东潍坊北港河口区的沉积物源于历史上黄河泥沙,目前的泥沙运动是由波浪造成的。
Through analysing the field data of the hydrologic and geomor-phic survey carried out inshore of weifang North Harbour during Spring and Fall 1990, it is concluded that the sediment in the estuarine area came from the Yellow River in history and the current sediment movement is.caused by wave.
出处
《海洋通报》
CAS
CSCD
北大核心
1992年第4期65-72,共8页
Marine Science Bulletin
关键词
沉积物
类型
泥沙
近海区
地形
Geomorphological features Sediment sources Inshore Weif-ang North Harbour
