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江西九江红土堆积的粒度特征及成因研究

李敬卫 乔彦松 王燕 彭莎莎

李敬卫, 乔彦松, 王燕, 等, 2009. 江西九江红土堆积的粒度特征及成因研究. 地质力学学报, 15 (1): 95-104.
引用本文: 李敬卫, 乔彦松, 王燕, 等, 2009. 江西九江红土堆积的粒度特征及成因研究. 地质力学学报, 15 (1): 95-104.
LI Jing-wei, QIAO Yan-song, WANG Yan, et al., 2009. AEOLIAN ORIGIN OF THE RED EARTH TORMATION IN JIUJIANG CITY OF JIANGXI PROVINCE, CHINA :EVIDENCE FROM GRAIN-SIZE ANALYSIS. Journal of Geomechanics, 15 (1): 95-104.
Citation: LI Jing-wei, QIAO Yan-song, WANG Yan, et al., 2009. AEOLIAN ORIGIN OF THE RED EARTH TORMATION IN JIUJIANG CITY OF JIANGXI PROVINCE, CHINA :EVIDENCE FROM GRAIN-SIZE ANALYSIS. Journal of Geomechanics, 15 (1): 95-104.

江西九江红土堆积的粒度特征及成因研究

基金项目: 

国家自然科学基金资助项目 40472088

中国地质调查局地质调查项目 1212010741403

地质力学研究所基本科研业务费项目 DZLXJK200711

详细信息
    作者简介:

    李敬卫(1970-), 男, 硕士研究生, 主要从事第四纪地质环境等方面研究工作。E-mail: lijingwei605@163.com

  • 中图分类号: P534.63

AEOLIAN ORIGIN OF THE RED EARTH TORMATION IN JIUJIANG CITY OF JIANGXI PROVINCE, CHINA :EVIDENCE FROM GRAIN-SIZE ANALYSIS

  • 摘要: 在南方红土的研究中, 区分不同地区红土地层的成因类型是研究区域古环境演化的关键。以江西九江红土剖面为例, 通过系统的粒度分析, 并与西峰黄土、古土壤样品及代表性河、湖相沉积的粒度特征进行对比, 结果表明, 九江红土与西峰黄土、古土壤样品具有相似的粒度分布特征, 而与河、湖相沉积有较大区别。其中, 九江剖面上部的下蜀土与西峰黄土粒度特征相近, 而剖面下部的网纹红土与西峰古土壤样品更为相似, 表明江西九江红土堆积与中国北方黄土一样属于风尘堆积。研究成果为古环境信息的进一步提取奠定了基础。

     

  • 图  1  九江红土与西峰黄土、古土壤及河、湖相沉积粒度分布的频率曲线

    图中(a)、(b)分别为九江剖面上部下蜀土和中、下部网纹红土样品; (c)、(d)分别为西峰黄土、古土壤样品; (e)为泸定湖相样品; (f)为宣城河流相样品

    Figure  1.  Grain-size distribution curves of the Jiujiang Red Earth, Xifeng loess and soil, lacustrine and fluvial sediment samples

    图  2  九江红土与西峰黄土、古土壤及河、湖相样品的粒度参数对比

    (a), (b) —九江剖面下蜀土及网纹红土样品; (c), (d) —西峰黄土、古土壤样品; (e) —泸定湖相样品; (f) —宣城河流相样品

    Figure  2.  Comparison of grain-size parameters among of the Jiujiang red earth, Xifeng loess, lacustrine and fluvial sediments

    图  3  九江红土与西峰黄土、古土壤以及河、湖相样品的粒度结构参数散点图

    ▽九江下蜀土; □九江网纹红土; △西峰黄土; +西峰古土壤; ○泸定湖相沉积; ▲宣城河流相沉积

    Figure  3.  Statistical parameters of grain-size distribution plots of the Jiujiang Red Earth, Xifeng loess and soil, lacustrine and fluvial sediments

    图  4  九江红土与西峰黄土、古土壤以及河、湖相样品的粒度指数图

    Figure  4.  Q1-Md-Q3 plots of the Jiujiang Red Earth, Xifeng loess and soil, lacustrine and fluvial sediments

    图  5  九江红土与西峰黄土、古土壤以及河、湖相样品的综合C-M图

    ▽九江下蜀土; □九江网纹红土; △西峰黄土; +西峰古土壤; ○泸定湖相沉积; ▲宣城河流相沉积

    Figure  5.  C-M plots of the Jiujiang Red Earth, Xifeng loess and soil, lacustrine and fluvial sediments

    图  6  九江红土与西峰黄土、古土壤以及河、湖相样品的判别参数

    Figure  6.  Y-values of grain-size distribution of the Jiujiang Red Earth, Xifeng loess and soil, lacustrine and fluvial sediments

    图  7  九江剖面粒度中值粒径及各粒级组分变化

    Figure  7.  Variations of median grain-size and some grain fractions content in Jiujiang section

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