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大渡河官料河昔木呷沟泥石流特征研究
引用本文:王小群,叶尚其,王兰生.大渡河官料河昔木呷沟泥石流特征研究[J].地质灾害与环境保护,2002,13(2):26-29,58.
作者姓名:王小群  叶尚其  王兰生
作者单位:1. 成都理工大学环境与土木工程学院,成都,610059
2. 四川省公路设计院,成都,610041
摘    要:根据工程地质分析的方法对大渡河官料河昔木呷沟泥石流的形成环境、基本特征、形成演化过程及机制模型、泥石流沟岸坡稳定性评价等进行了分析,并对泥石流活动趋势做出科学的评价预测。对工程建设中的泥石流分析有着积极的指导作用。

关 键 词:昔木呷沟  泥石流  形成机制  岸坡  稳定性  地貌
文章编号:1006-4362(2002)02-0026-04

ANALYSIS OF DEBRIS FLOW CHARACTERISTICS OF THE XIMUXIA GULLY IN THE BRANCH OF DADU RIVER
WANG Xiao-qun ,YE Shang-qi ,WANG Lan-sheng.ANALYSIS OF DEBRIS FLOW CHARACTERISTICS OF THE XIMUXIA GULLY IN THE BRANCH OF DADU RIVER[J].Journal of Geological Hazards and Environment Preservation,2002,13(2):26-29,58.
Authors:WANG Xiao-qun  YE Shang-qi  WANG Lan-sheng
Institution:WANG Xiao-qun 1,YE Shang-qi 2,WANG Lan-sheng 1
Abstract:In this paper,the authors analyse the formation conditions,basic characteristics and the formation and evolution steps of the Ximuxia gully debris flow in the branch(Guanliao river)by the engineering geology analysis.The authors evaluate the mechanism model and the slope stability of the debris flow gully and makes a scientific prediction for the trend of the debris flow activities.This has an active guiding meaning in analysing the debris flows in engineering constructions.
Keywords:Ximuxia gully  debris flow  formation evolution  mechanism model
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