黄河上游拉干峡—寺沟峡段特大型滑坡 及其成因研究
DOI:
作者:
作者单位:

作者简介:

通讯作者:

中图分类号:

基金项目:

本文为国家自然科学基金(批准号 41302253),国家重点基础研究发展计划项目(973)(批准号 2014CB744702),“十二五”国家科技支撑项目(批准号 2012BAK10B01)和青海省自然科学基金(批准号 2012 Z 936Q)的成果。


Research on Large scale Landslides between Lagan Gorge and Sigou Gorge in the Upper Reaches of Yellow River
Author:
Affiliation:

Fund Project:

单位:
  • 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:

    黄河上游拉干峡—寺沟峡段共发育特大型滑坡116处,群尖盆地无论是数量还是强度上都占到了绝对优势,这与其所处的特殊构造部位和昆黄运动时期各大断裂带运动性质的转变直接相关;高原掀斜式隆升过程导致各大支流水系特大型滑坡西岸多发于东岸。研究区特大型滑坡有明显的4个群发期,各期都有其不同的触发因素,50 ka和30 ka属构造和气候的耦合成因,10 ka为构造触发, 5 ka 为降雨所致。

    Abstract:

    116 large scale landslides develop between Lagan Gorge and Sigou Gorge in the upper reaches of the Yellow River. And there, Qunjian basin has an edge over others in quantity and intensity of landslide events, as has a direct correlation with the unique tectonic position and the characteristic change of the major fracture zone during Kun Huang movement epoch. The tilting uplift process of plateau causes more large scale landslides to occur in the west coast than the east coast along the major tributaries of river systems. Large scale landslides were triggered by the respective factors during 4 distinct phases, i.e. before 50km and 30km for the coupling cause of tectonic and climatic, before 10km by tectonic, and before 5km by rainfall.

    参考文献
    相似文献
    引证文献
引用本文

周保,彭建兵,殷跃平,李小林,魏刚,马小强.2014.黄河上游拉干峡—寺沟峡段特大型滑坡 及其成因研究[J].地质论评,60(1):138-144,[DOI].
.2014. Research on Large scale Landslides between Lagan Gorge and Sigou Gorge in the Upper Reaches of Yellow River[J]. Geological Review,60(1):138-144.

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:2013-01-22
  • 最后修改日期:2013-12-06
  • 录用日期:
  • 在线发布日期: 2014-01-17
  • 出版日期: