黄土高原重力侵蚀的地质地貌因素分析--从发生的规模频度看区域特征
DOI:
作者:
作者单位:

作者简介:

通讯作者:

中图分类号:

基金项目:

日本国际交流基金(JPF)2005年度研究奖学金“中国黄土高原水土流失与人们生活关系研究”


Geological and Geomorphological Conditions of Mass Movements in the Loess Plateau--Regional Characteristics From the Viewpoint of Magnitude and Frequency of Event Occurrence
Author:
Affiliation:

Fund Project:

  • 摘要
  • |
  • 图/表
  • |
  • 访问统计
  • |
  • 参考文献
  • |
  • 相似文献
  • |
  • 引证文献
  • |
  • 资源附件
  • |
  • 文章评论
    摘要:

    在按规模和频度对黄土高原重力侵蚀分类的基础上,分析了重力侵蚀具有普遍性、沿河谷分布、区域差异明显等区域分布特点。并分析了地质地貌因素对各种主要重力侵蚀形成与分布的影响:塌陷在碳酸盐地层存在地分布较多,高陡边坡地区易于形成巨大滑坡,群发性崩塌、滑坡以及泥流的形成多发生在沟谷密度较大地区,巨大泥流的形成在沟头地区多有较大的汇水面积等。因此在防治重力侵蚀过程中,必须充分地研究各地的地质地貌条件,因地制宜地防治不同类型的重力侵蚀。

    Abstract:

    The authors investigated the distribution of mass movements in the Loess Plateau by means of field survey and mapping based on the magnitude and frequency of them.We found the following regional characteristics of mass movement occurrence:(1) mass movements broadly occur along river valleys in the Loess Plateau;(2) the occurrence obviously shows regional difference;(3) the geological and geomorphological conditions strongly affect the occurrence and distribution of mass movements.For instance,sink holes mainly occur at the place where carbonate rock exists,large landslides occur along the cliffs that have a great altitudinal difference,small and frequent landslides and mud flows occur at the place where drainage density is high,and great mud flows occur with the large drainage area.These results indicate that the geological and geomorphological conditions must be considered in order to prevent mass movements in the Loess Plateau.

    参考文献
    相似文献
    引证文献
引用本文

松永光平,甘枝茂.黄土高原重力侵蚀的地质地貌因素分析--从发生的规模频度看区域特征[J].水土保持通报,2007,(1):55-57,91

复制
分享
文章指标
  • 点击次数:
  • 下载次数:
  • HTML阅读次数:
  • 引用次数:
历史
  • 收稿日期:2006-07-11
  • 最后修改日期:2006-09-25
  • 录用日期:
  • 在线发布日期: 2014-11-26
  • 出版日期: