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    江汉平原沉积物重矿物特征及其对三峡贯通的指示

    康春国 李长安 王节涛 邵磊

    康春国, 李长安, 王节涛, 邵磊, 2009. 江汉平原沉积物重矿物特征及其对三峡贯通的指示. 地球科学, 34(3): 419-427.
    引用本文: 康春国, 李长安, 王节涛, 邵磊, 2009. 江汉平原沉积物重矿物特征及其对三峡贯通的指示. 地球科学, 34(3): 419-427.
    KANG Chun-guo, LI Zhang-an, WANG Jie-tao, SHAO Lei, 2009. Heavy Minerals Characteristics of Sediments in Jianghan Plain and Its Indication to the Forming of the Three Gorges. Earth Science, 34(3): 419-427.
    Citation: KANG Chun-guo, LI Zhang-an, WANG Jie-tao, SHAO Lei, 2009. Heavy Minerals Characteristics of Sediments in Jianghan Plain and Its Indication to the Forming of the Three Gorges. Earth Science, 34(3): 419-427.

    江汉平原沉积物重矿物特征及其对三峡贯通的指示

    基金项目: 

    国家重点基础研究973发展计划 2004CB720204

    国家自然科学基金 40672206

    详细信息
      作者简介:

      康春国(1968-), 男, 博士研究生, 副教授, 第四纪地质学专业.E-m ail: chunguokang@sohu.com

      通讯作者:

      李长安, E-mail: chanli@cug.edu.cn

    • 中图分类号: P571

    Heavy Minerals Characteristics of Sediments in Jianghan Plain and Its Indication to the Forming of the Three Gorges

    • 摘要: 江汉平原是长江穿过三峡区的第一个大型卸载盆地, 其沉积物必然反映长江流经的物源区的物源特征.通过对盆地中心周老孔第四纪岩心的重砂样品中0.125~0.063mm粒级的重矿物含量变化、ATi、GZi、ZTR指数和重矿物组合分析, 发现从钻孔岩心深度110m开始向上, 水动力条件加强, 沉积速率加快, 重矿物的数量特征发生明显突变, 特征矿物的组合与现代长江相同.表明在周老孔岩心深度110m (古地磁年龄1.1Ma左右) 位置处, 长江三峡开始贯通, 江汉平原开始接纳长江带来的三峡上游的物质.

       

    • 图  1  江汉平原周老孔位置

      Fig.  1.  Study map and location of Zhoulao core in the Jianghan plain

      图  2  周老孔岩性柱、古地磁及重矿物含量变化曲线综合

      图中极性柱引自文献张玉芬等(2008); 图中各种重矿物的含量均为1/万

      Fig.  2.  Lithologic column, paleomagnetism and curves of main heavy minerals content variation of Zhoulao core

      图  3  主要重矿物含量的平均值

      Fig.  3.  Average content of main heavy minerals

      图  4  ATi指数、GZi指数、ZTR指数及主要重矿物之和的含量变化曲线

      Fig.  4.  Curves of ATi, GZi, ZTR and sum of main heavy minerals content variation

      图  5  重矿物重量平均含量变化

      Fig.  5.  Average weight content variations of heavy minerals

      图  6  长江流域岩性分布

      根据中科院长春地理研究所《长江流域水体环境背景值研究图集》(1998), 重新绘制

      Fig.  6.  Distributions of lithology in the Yangtze River basin

      表  1  周老孔岩心(0.063~0.125 mm)粒级各样品中重矿物种类及含量随深度变化对比(重矿物含量单位: 1/万)

      Table  1.   Heavy minerals contents of samples (in 0.063-0. 125 mm size fraction) varying with depth in Zhoulao Core

      表  2  ATi指数、GZi指数、ZTR指数及主要重矿物之和的含量

      Table  2.   ATi, GZi, ZTR and sum of main heavy minerals content

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