连云港洪门古沙堤沉积特征及其意义

徐军, 殷勇, 朱大奎, 朱小兵. 连云港洪门古沙堤沉积特征及其意义[J]. 海洋地质与第四纪地质, 2007, 27(1): 23-35.
引用本文: 徐军, 殷勇, 朱大奎, 朱小兵. 连云港洪门古沙堤沉积特征及其意义[J]. 海洋地质与第四纪地质, 2007, 27(1): 23-35.
XU Jun, YIN Yong, ZHU Da-kui, ZHU Xiao-bing. SEDIMENTARY CHARACTERISTICS AND ENVIRONMENTAL SIGNIFICANCE OF HONGMEN COASTAL BARRIER,LIANYUNGANG, NORTHEASTERN JIANGSU PROVINCE[J]. Marine Geology & Quaternary Geology, 2007, 27(1): 23-35.
Citation: XU Jun, YIN Yong, ZHU Da-kui, ZHU Xiao-bing. SEDIMENTARY CHARACTERISTICS AND ENVIRONMENTAL SIGNIFICANCE OF HONGMEN COASTAL BARRIER,LIANYUNGANG, NORTHEASTERN JIANGSU PROVINCE[J]. Marine Geology & Quaternary Geology, 2007, 27(1): 23-35.

连云港洪门古沙堤沉积特征及其意义

  • 基金项目:

    江苏省自然科学基金项目(BK2002089)

    国家自然科学基金项目(40271004)

详细信息
    作者简介: 徐军(1967-),女,副教授,南京大学在读博士,专业为海岸带资源与环境
  • 中图分类号: P736.21

SEDIMENTARY CHARACTERISTICS AND ENVIRONMENTAL SIGNIFICANCE OF HONGMEN COASTAL BARRIER,LIANYUNGANG, NORTHEASTERN JIANGSU PROVINCE

  • 通过钻孔、年代地层、沉积物粒度和有孔虫组合综合分析,并配合探地雷达,对洪门古沙堤的成因类型以及古海岸环境进行了探讨。洪门古沙堤沉积物和海州湾现代沙滩、苏北平原贝壳堤相比较,颗粒集中在粗砂-极粗砂范围,分选性偏差,极有可能形成于靠近河口或受河口影响的环境。探地雷达揭示洪门古沙堤曾有过向海方向的进积和生长,指示当时沙源丰富。洪门古沙堤的浅钻地层反映了洪门地区在6 400 aBP左右为滨海沼泽环境,此时期与青莲岗文化期的年代相吻合;湖沼沉积结束后,洪门地区迎来了中全新世的最大海侵,受周围地形的制约,洪门地区可能形成了河口浅海湾环境,普遍沉积了2 m左右的青灰色淤泥沉积,有孔虫组合反映当时的环境并非完全开敞,而是受到一定程度限制的近岸浅水环境,反映了洪门地区为浅海湾环境;6 000 aBP左右,随着砂砾质沉积物供应的丰富以及相对海平面下降,洪门古沙堤开始发育,直到5 000 aBP苏北和连云港地区普遍发生海退,古沙堤发育结束。
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出版历程
收稿日期:  2006-08-02
修回日期:  2006-12-10

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