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麻柳沟危岩体的形成机制与稳定性分析
引用本文:张青宇,沈军辉,陈明东,刘海.麻柳沟危岩体的形成机制与稳定性分析[J].地质灾害与环境保护,2011,22(1):98-102.
作者姓名:张青宇  沈军辉  陈明东  刘海
作者单位:张青宇,沈军辉,刘海,Zhang Qing-yu,Shen Jun-hui,Liu Hai(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,成都,610059);陈明东,Chen Ming-dong(浙江省第十一地质大队西南地质工程研究院,成都,610059)
摘    要:为促进危岩体的防治和"5.12"地震后的重建工作,以青川麻柳沟危岩体为例,从地质结构、地形地貌和变形特征三方面探讨危岩体的形成机制.然后通过定性的野外调查和定量的极限平衡法分析危岩体稳定性.结果表明.麻柳沟危岩体形成于压致蠕变一拉裂作用,以倾倒式破坏为主,三个危岩体中,一个欠稳定,另两个稳定.

关 键 词:危岩体  地质结构  形成机制  稳定性

FORMATION MECHANISM AND STABILITY OF THE DANGEROUS ROCK-MASSES IN MALIU GULLY
Zhang Qing-yu,Shen Jun-hui,Chen Ming-dong,Liu Hai.FORMATION MECHANISM AND STABILITY OF THE DANGEROUS ROCK-MASSES IN MALIU GULLY[J].Journal of Geological Hazards and Environment Preservation,2011,22(1):98-102.
Authors:Zhang Qing-yu  Shen Jun-hui  Chen Ming-dong  Liu Hai
Institution:1(1.Geological Hazards Prevention and Geological Environment Protection,Chengdu University of Technology,Chengdu 610059,China;2.Zhejiang 11th Geological Battalion Southwest Geological Engineering Research Institute,Chengdu 610059,China)
Abstract:To promote the prevention and treatment of dangerous rock-masses and the reconstruction after the May 12-th Earthquake,their formation mechanism is explored.As a case,the dangerous rock-masses in Maliu Gully,Qingchuan,are studied in terms of topography,geological structure and deformation characteristics.And their stability is analyzed,based on the qualitative field investigations and the quantitative limit-equilibrium studies.The results show that the masses resulted from pressure-induced creep-crack with the dumping type in the main and only one unstable of the three.
Keywords:Dangerous rock-mass  Geologic structure  Formation mechanism  Stability
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