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    基于磁组构特征的江汉平原全新世古洪水事件

    张玉芬 李长安 陈亮 王辉

    张玉芬, 李长安, 陈亮, 王辉, 2009. 基于磁组构特征的江汉平原全新世古洪水事件. 地球科学, 34(6): 985-992.
    引用本文: 张玉芬, 李长安, 陈亮, 王辉, 2009. 基于磁组构特征的江汉平原全新世古洪水事件. 地球科学, 34(6): 985-992.
    ZHANG Yu-fen, LI Zhang-an, CHEN Liang, WANG Hui, 2009. Magnetic Fabric of Holocene Palaeo-Floods Events in Jianghan Plain. Earth Science, 34(6): 985-992.
    Citation: ZHANG Yu-fen, LI Zhang-an, CHEN Liang, WANG Hui, 2009. Magnetic Fabric of Holocene Palaeo-Floods Events in Jianghan Plain. Earth Science, 34(6): 985-992.

    基于磁组构特征的江汉平原全新世古洪水事件

    基金项目: 

    国家自然科学基金项目 40472151

    国家自然科学基金项目 40672206

    国家自然科学基金项目 40771213

    国家重点基础研究发展计划(“973”计划) 2004CB720204

    详细信息
      作者简介:

      张玉芬(1957-), 女, 教授, 博士, 主要从事环境地球物理等方面的教学与研究.E-mail: zhyfcug@163.com

    • 中图分类号: P584;X143

    Magnetic Fabric of Holocene Palaeo-Floods Events in Jianghan Plain

    • 摘要: 在对江汉平原江陵剖面全新世沉积物的沉积环境和年代学分析的基础上, 利用由现代洪水沉积所建立的洪泛沉积物磁组构参数标志, 对江汉平原全新世以来的古洪水事件进行了初步研究.结果表明: (1) 江汉平原全新世以来(有史料记载前), 共有55个特大洪水沉积层(事件). (2) 全新世以来特大洪水(期) 演化可分为两个大的阶段: 第一阶段(9875~3000aBP) 低频期, 该阶段洪水发生频率不高, 且洪水周期比较稳定, 主要以近千年和500~625a周期为主; 第二阶段(3000aBP~现在) 为洪水频发期.洪水发生的周期以300~200a为主, 反映出洪水发生的频率具有加快的趋势.

       

    • 图  1  研究区交通及剖面位置图

      Fig.  1.  The transportation and section position of the research area

      图  2  江陵剖面岩性柱及部分磁组构参数变化曲线

      Fig.  2.  Lithology column and variation curves of magnetic susceptibility parameters along with depth for Jiangling profile in Hubei Province

      图  3  江陵剖面古洪水事件(期) 的识别结果

      图中以箭头方向代表长轴主方向倾向即长轴的偏角方向, 箭头长短代表长轴主方向倾角大小

      Fig.  3.  Palaeo-floods events (period) distinguished from sediment of Jiangling section

      图  4  江汉平原近1万年来洪水频率曲线图

      a图为9 875~3 000 aBP时段; b图为3 000~639 aBP时段

      Fig.  4.  Late 10 000 a floodwater frequency curve map in Jianghan plain

      表  1  14C测年数据

      Table  1.   Dating data of the radiocarbon age

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    • 收稿日期:  2008-12-12
    • 刊出日期:  2009-11-25

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