长江口各地貌单元沉积构造和粒度分区特征

喻薛凝, 战庆, 王张华. 长江口各地貌单元沉积构造和粒度分区特征[J]. 海洋地质与第四纪地质, 2016, 36(4): 1-11. doi: 10.16562/j.cnki.0256-1492.2016.04.001
引用本文: 喻薛凝, 战庆, 王张华. 长江口各地貌单元沉积构造和粒度分区特征[J]. 海洋地质与第四纪地质, 2016, 36(4): 1-11. doi: 10.16562/j.cnki.0256-1492.2016.04.001
YU Xuening, ZHAN Qing, WANG Zhanghua. SEDIMENTARY STRUCTURES AND GRAIN SIZE PATTERNS OF THE GEOMORPHIC UNITS IN THE YANGTZE RIVER MOUTH[J]. Marine Geology & Quaternary Geology, 2016, 36(4): 1-11. doi: 10.16562/j.cnki.0256-1492.2016.04.001
Citation: YU Xuening, ZHAN Qing, WANG Zhanghua. SEDIMENTARY STRUCTURES AND GRAIN SIZE PATTERNS OF THE GEOMORPHIC UNITS IN THE YANGTZE RIVER MOUTH[J]. Marine Geology & Quaternary Geology, 2016, 36(4): 1-11. doi: 10.16562/j.cnki.0256-1492.2016.04.001

长江口各地貌单元沉积构造和粒度分区特征

  • 基金项目:

    国土资源部公益项目(201211009)

详细信息
    作者简介: 喻薛凝(1990-),男,硕士生,主要从事海洋沉积学研究,E-mail:yuxuening@126.com
  • 中图分类号: P737.1

SEDIMENTARY STRUCTURES AND GRAIN SIZE PATTERNS OF THE GEOMORPHIC UNITS IN THE YANGTZE RIVER MOUTH

  • 根据165个柱状样顶部1 m的沉积构造和粒度分析结果,对长江口各地貌单元的沉积物特征进行了规律性总结,以应用于钻孔沉积相的判断。结果显示,河口心滩、上河口段落潮槽和拦门沙为主要砂质沉积区,属于牵引流沉积,分粒级频率曲线的峰值主要出现在63~125 μm及125~250 μm粒级,且峰值在125~250 μm粒级的样品向海逐渐增多。而残留砂沉积物粒径大、分选好,特征明显。其余地貌单元均以泥质沉积为主,典型特征有:(1)潮坪层偶发育,砂质纹层密集;(2)在分粒级频率曲线中,口内涨潮槽主峰以μm为主,口外涨潮槽变粗为31~63 μm占主导,且砂质薄层增多;(3)下河口段落潮槽纹层很多,极薄纹层占主导;(4)南汇边滩分粒级曲线常见双峰现象,平均中值粒径在泥质沉积区最大,部分沉积物位于C-M图的递变悬浮段;(5)三角洲前缘复式河槽沉积物明显细于其他前缘沉积,反映了滞流点附近的弱水动力特征;(6)前三角洲为均质泥,纹层少见,为长江口区最细的沉积。
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收稿日期:  2015-12-21
修回日期:  2016-03-28

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