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汶川大地震山地灾害发育的控制因素分析

ANALYSIS OF THE CONTROLLING FACTORS ON GEO-HAZARDS IN MOUNTAINOUS EPICENTER ZONES OF THE WENCHUAN EARTHQUAKE

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【作者】 王运生罗永红吉峰霍俊杰吴峻峰徐鸿彪

【Author】 WANG Yunsheng LUO Yonghong JI Feng HUO Junjie WU Junfeng XU Hongbiao(State Key Laboratory of Geo-Hazard Prevention and Geo-Environment Protection,Chengdu University of Technology,Chengdu 610059)

【机构】 成都理工大学地质灾害防治与地质环境保护国家重点实验室

【摘要】 汶川大地震震后地质灾害调查结果表明,龙门山山地灾害无论是空间分布还是在剖面分布上均具有明显的不均一性:平面上集中在发震断裂及非发震断裂及其附近,剖面上集中在坡顶、坡折及孤立的突出地形上;运动形式具有加速起飞-滑翔-俯冲着陆三阶段。主要受控因素有发震断裂、高烈度、地震持续时间、斜坡地形效应、岩性及结构等。

【Abstract】 Our reconnaissance to the mountainous epicenter zones of the Wenchuan Earthquake shows that the geohazard distribution in the Longmen Shan is heterogeneous on both horizontal and vertical directions.The geohazards are concentrated along the seismic fractures and non-seismic fractures in horizontal and at the top,river shoulders and isolated topography in vertical.The movement process can be divided into three stages of zero-length accelerated launching,gliding and-landing.The development of the geo-hazards is controlled by the seismic fracture,high intensity,duration of the earthquake,topography effects,the composed lithology and textures of the mountainous slopes.

【基金】 国家自然科学基金(40472143,D0214);国家重点基础研究发展计划课题“强震作用下斜坡失稳破坏机理及分布规律”(2008CB425801)资助
  • 【文献出处】 工程地质学报 ,Journal of Engineering Geology , 编辑部邮箱 ,2008年06期
  • 【分类号】P694
  • 【被引频次】74
  • 【下载频次】493
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