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郑州邙山官庄峪黄土地层研究

王玉振 王书兵 王喜生 傅建利 蒋复初

王玉振, 王书兵, 王喜生, 等, 2015. 郑州邙山官庄峪黄土地层研究. 地质力学学报, 21 (3): 393-398.
引用本文: 王玉振, 王书兵, 王喜生, 等, 2015. 郑州邙山官庄峪黄土地层研究. 地质力学学报, 21 (3): 393-398.
WANG Yu-zhen, WANG Shu-bing, WANG Xi-sheng, et al., 2015. STUDY ON THE GUANZHUANGYU LOESS STRATIGRAPHY IN MANGSHAN, ZHENGZHOU. Journal of Geomechanics, 21 (3): 393-398.
Citation: WANG Yu-zhen, WANG Shu-bing, WANG Xi-sheng, et al., 2015. STUDY ON THE GUANZHUANGYU LOESS STRATIGRAPHY IN MANGSHAN, ZHENGZHOU. Journal of Geomechanics, 21 (3): 393-398.

郑州邙山官庄峪黄土地层研究

基金项目: 

中国地质科学院重点开放实验室专项资金资助项目 KL05-13

国家自然科学基金项目 40302025

国家自然科学基金项目 40642001

详细信息
    作者简介:

    王玉振(1961-), 男, 高级工程师。主要从事水文水资源分析与评价工作。E-mail:xyjwyz@126.com

    通讯作者:

    王书兵(1972-), 男, 副研究员。主要从事第四纪地质与环境研究工作。E-mail:wsbln@126.com

  • 中图分类号: P642.13

STUDY ON THE GUANZHUANGYU LOESS STRATIGRAPHY IN MANGSHAN, ZHENGZHOU

  • 摘要: 邙山官庄峪剖面共厚154.9 m, 出露S10及以上黄土-古土壤地层序列, 特征的马兰黄土厚度达70.125 m, 具有明显的粗粒、均匀特点, 且在该段地层中部, 并没有比较明显的弱古土壤层。磁性地层测量表明B/M界线置于深度132.04 m处, 位于L8的下部; 剖面底部未进入Jaramillo正极性亚时。与赵下峪剖面对比结果显示, 以B/M界线为标志, 72 m以下地层两者高度一致, 只是对地层的划分不同而已; 但赵下峪剖面中比较特征的具有较高磁化率值的L1SS1地层单元, 在官庄峪剖面却无明显表现, 其原因可能需进一步深入研究。

     

  • 图  1  郑州邙山官庄峪黄土-古土壤剖面磁性地层序列

    Figure  1.  Magnetic stratigraphic sequence of Guanzhuangyu loess-paleosol profile in Mangshan, Zhengzhou

    图  2  邙山官庄峪黄土-古土壤剖面下部B/M磁性地层序列

    Figure  2.  The B/M magnetic stratigraphic sequence below Guangzhuangyu loess-paleosol profile

    图  3  邙山官庄峪黄土剖面与赵下峪黄土剖面地层对比

    Figure  3.  Stratigraphy comparison between Guanzhuangyu loess and Zhaoxiayu loess profiles in Mangshan

    图  4  邙山官庄峪黄土剖面磁性地层与赵下峪黄土剖面磁性地层对比

    Figure  4.  Magnetostratigraphy comparison between Guanzhuangyu loess and Zhaoxiayu loess profiles in Mangshan

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出版历程
  • 收稿日期:  2015-02-19
  • 刊出日期:  2015-09-28

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