连云港近岸海域沉积物特征与沉积环境

范恩梅, 陈沈良, 张国安. 连云港近岸海域沉积物特征与沉积环境[J]. 海洋地质与第四纪地质, 2009, 29(2): 33-40. doi: 10.3724/SP.J.1140.2009.02033
引用本文: 范恩梅, 陈沈良, 张国安. 连云港近岸海域沉积物特征与沉积环境[J]. 海洋地质与第四纪地质, 2009, 29(2): 33-40. doi: 10.3724/SP.J.1140.2009.02033
FAN Enmei, CHEN Shenliang, ZHANG Guoan. SEDIMENT CHARACTERISTICS AND SEDIMENTARY ENVIRONMENT IN LIANYUNGANG COASTAL WATERS[J]. Marine Geology & Quaternary Geology, 2009, 29(2): 33-40. doi: 10.3724/SP.J.1140.2009.02033
Citation: FAN Enmei, CHEN Shenliang, ZHANG Guoan. SEDIMENT CHARACTERISTICS AND SEDIMENTARY ENVIRONMENT IN LIANYUNGANG COASTAL WATERS[J]. Marine Geology & Quaternary Geology, 2009, 29(2): 33-40. doi: 10.3724/SP.J.1140.2009.02033

连云港近岸海域沉积物特征与沉积环境

  • 基金项目:

    河口海岸学国家重点实验室科研业务项目(2008KYYW06)

    我国近海海洋综合调查与评价项目(908-01-ZH2,908-02-03-04)

详细信息
    作者简介: 范恩梅(1982-),女,硕士生,主要从事海岸动力沉积与工程应用研究,E-mail:enmfan@163.com
  • 中图分类号: P737.2

SEDIMENT CHARACTERISTICS AND SEDIMENTARY ENVIRONMENT IN LIANYUNGANG COASTAL WATERS

  • 根据连云港地区近岸海域的表层沉积物分析结果,运用Flemming的三角图示对沉积环境进行划分,并在此基础上结合沉积物结构、地形及水动力条件,探讨了研究区域沉积物特征及沉积环境。结果表明,研究区域沉积物以潮流作用为主,沉积环境可划分为近岸和远岸沉积环境。近岸沉积环境,由于潮流由外海向岸逐渐减小,向上部搬运的泥沙粒径越来越小,因此该区域泥沙颗粒较细,主要为黏土质粉砂和砂-粉砂-黏土;远岸沉积环境,潮流流速很大,可掀动并搬运较细颗粒泥沙,使得远岸区域有进一步粗化的趋势。
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出版历程
收稿日期:  2008-12-13
修回日期:  2009-02-24

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