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炉城镇柳杨沟泥石流灾害及其形成条件探讨
引用本文:刘岁海.炉城镇柳杨沟泥石流灾害及其形成条件探讨[J].水土保持研究,2007,14(2):182-183.
作者姓名:刘岁海
作者单位:西南科技大学城建学院, 四川, 绵阳, 621010
摘    要:康定县地处川西平原与四川盆周的过渡地带,县域内地势险峻,地形切割强烈,地层与地质构造复杂,新构造运动强烈,地震活动频繁,泥石流、滑坡、崩塌等地质灾害十分发育。作者通过收集资料与现场调查,分析研究了康定县城一典型泥石流——柳杨沟泥石流的活动概况、危害、形成条件及其形成机制,并对防治对策提出了建议。

关 键 词:泥石流  形成条件  炉城镇柳杨沟
文章编号:1005-3409(2007)02-0182-02
收稿时间:2006-04-04
修稿时间:2006年4月4日

Debris Flow Hazards and Its Formation in Liuyang Gully of Lucheng Town
LIU Sui-hai.Debris Flow Hazards and Its Formation in Liuyang Gully of Lucheng Town[J].Research of Soil and Water Conservation,2007,14(2):182-183.
Authors:LIU Sui-hai
Institution:City Construction School, Southwest University of Science and Technology, Mianyang, Sichuan 621010, China
Abstract:Kangding County is located in transition belt of Sichuan west plain and Sichuan basin. In this field,terrain is steep, landform incision is fierce,stratum and geological structure is complex, neotectonic movement is strong,earthquake activity is frequent, geological hazards debris flow, landslide and collapse develop strongly. Through collecting data and thorough survey on the spot, the author analyses and studies the general situation, harm, formation conditions and mechanism of the debris flow in Liuyang gully of Lucheng town,and brings forward primary suggestion for its prevention and control.
Keywords:debris flow  formation conditions  Liuyang gully of Lucheng town
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