| 川主寺尕里台滑坡形成机制分析 |
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| 引用本文： | 王影,陈国辉,钟声,王晓东.川主寺尕里台滑坡形成机制分析[J].四川地质学报,2009,29(4):446-448. |
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| 作者姓名： | 王影 陈国辉 钟声 王晓东 |
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| 作者单位： | 四川省地质工程勘察院,成都,610072 |
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| 摘 要： | 尕里台滑坡位于松潘县北西约39km，在哲波河上游尕里台支沟右岸Ⅰ级阶地边缘谷坡中下部，为体积约10×10^4m^3的中型滑坡。滑坡体在天然或暴雨状态下处于不稳定状态，现根据所掌握的资料，对滑坡形成机制进行分析。
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| 关 键 词： | 滑坡 形成机制 诱发作用 尕里台 |
Genetic Mechanism for the Galitai Landslide at the Chuanzhu Temple |
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| WANG Ying,CHEN Guohui,ZHONG Sheng,WANG Xiaodong.Genetic Mechanism for the Galitai Landslide at the Chuanzhu Temple[J].Acta Geologica Sichuan,2009,29(4):446-448. |
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| Authors: | WANG Ying CHEN Guohui ZHONG Sheng WANG Xiaodong |
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| Institution: | (Sichuan Research Institute of Engineering Exploration, Chengdu 610072) |
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| Abstract: | The Galitai landslide is located at about 39 km northwest of Songpan County Town, lying in the middle-lower part of terrace Ⅰ of the right bank of the Galitai valley in the upper reaches of the Zhebo River with the volume of about 10 × 10^4m^3. This paper makes an approach to the genetic mechanism for the landslide. |
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| Keywords: | landslide genetic mechanism inducing factor Galitai |
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