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长江口北支潮流沙体沉积物来源分析
引用本文:周开胜,孟翊,刘苍字,洪雪晴.长江口北支潮流沙体沉积物来源分析[J].海南师范大学学报(自然科学版),2007,20(3):277-282.
作者姓名:周开胜  孟翊  刘苍字  洪雪晴
作者单位:1. 蚌埠学院食品与生物工程系,安微蚌埠,233030
2. 华东师范大学河口海岸国家重点实验室,上海,200062
3. 华东师范大学地理系,上海,200062
基金项目:国家自然科学基金项目(40676028),国家自然科学基金青年基金项目(40206013)
摘    要:通过对兴隆沙地区沉积物环境磁学特征分析,发现该地区磁性矿物主要以来源于长江亚铁磁性矿物为主,并含有少量的反铁磁性矿物;通过微体古生物特征分析,发现长江口北支沉积物主要由潮流流携带而来.综合环境磁学和微体古生物学特征,得出该地区沉积物的来源是多源的,以长江源为主.

关 键 词:长江口北支  潮流沙体  沉积物来源

Analysis of the source of tidal sandy sediments in the north branch of Changjiang River esturary
Zhou Kaisheng,Meng Yi,Liu Cangzi,Hong Xueqing.Analysis of the source of tidal sandy sediments in the north branch of Changjiang River esturary[J].Journal of Hainan Normal University:Natural Science,2007,20(3):277-282.
Authors:Zhou Kaisheng  Meng Yi  Liu Cangzi  Hong Xueqing
Abstract:Through an analysis of the magnetic characteristic on Xinglongsha Island, it is discovered that the ferrous magnetic mineral is mainly from Changjiang River.By analyzing the features of foraminifer, we find that the sedimental substance at the north branch of Changjiang River stems from torrents and tides along the coast of north Jiangsu. In view of the features of the environmental magnetics and of foraminifera, it is concludled that the source of the sedimental substance in that region larea is varied, with that of Changjrang River as the dominant one.
Keywords:the north branch of Changjiang River estuary  the tidal sandy sediments  the source of sediments
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