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兴仁围豹滑坡形成条件及诱发机制探讨

Formation conditions and inducing mechanism of Xingren Weibao Landslide
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摘要 在亚热带暖温湿润季风气候区,以兴仁围豹滑坡为研究对象,探讨含软弱夹层的顺层滑坡的形成条件及诱发机制。通过实地调查滑坡所在地区的自然地理、气候水文、地形地貌、工程地质、地质构造等有直接影响的环境条件,运用理论综合分析探讨围豹滑坡诱发机制,结果表明:围豹滑坡形成原因为特定的环境条件及人类活动,雨水入渗软化滑动面及静水压力相互作用诱发滑坡。 Taking Xingren Weibao Landslide as the research object,the formation conditions and inducing mechanism of the bedding landslide with weak intercalation are analyzed.Through field investigation of the physical geography,climate,hydrology,landform,engineering geology,geological structure,etc.in the landslide area,the inducing mechanism of Weibao Landslide is discussed comprehensively.The results show that the reason for Weibao Landslide is the specific environment conditions and human activities;the interaction of rainfall infiltration and static water pressure has induced the landslide.
作者 陈寿稀 廖德武 兰中孝 郑冰 杜艳松 王源 CHEN Shouxi;LIAO Dewu;LAN Zhongxiao;ZHENG Bing;DU Yansong;WANG Yuan(Guizhou Geology and Mineral Foundation Engineering Co.Ltd.,Guiyang 550081,China;Institute of Geophysical and Geochemical Exploration,Guizhou Provincial Bureau of Geology and Mineral Exploration and Development,Guiyang 550018,China)
出处 《贵州科学》 2022年第4期72-76,共5页 Guizhou Science
基金 贵州省科技计划(社会攻关计划)项目(黔科合SY字[2015]3057) 黔地矿科合[2017]36号。
关键词 兴仁围豹滑坡 形成条件 诱发机制 软弱夹层 顺层滑坡 Xingren Weibao Landslide formation conditions inducing mechanism weak intercalation bedding landslide
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