清西陵云蒙山泥石流的地质特征  

GEOLOGICAL CHARACTERISTICS OF MUD-ROCK FLOW IN YUNMENG MOUNTAIN IN THE REGION OF WEST TOMBS OF QING DYNASTY

作　　者：安光义[1] 王桂霞[1] 

机构地区：[1]河北农业大学,河北保定071000

出　　处：《河北林果研究》2003年第2期145-148,共4页Hebei Journal of Forestry and Orchard Research

摘　　要：在野外调查的基础上,探讨了清西陵地区云蒙山泥石流发育的岩石特征、山体构造,泥石流形成的地形、地貌特征、运动路线和搬运物沉积的位置,该区发育的泥石流类型,搬运后沉积物的地质特征。认为该区地貌上形成泥石流堆积扇和平行状垄岗。为有效地保护陵区、指导区内农牧业生产和村落选址提出了合理的建议。Based on field investigations of mud-rock flow originated petrographical characteristics, mountain structure,topography and geomorphology are discussed in this paper. And the moving route,seat of deposit together with the geological characteristics of the deposit are also given.After the taking place of mud-rock flow,fun-shaped depoist and paralleled ridge-and-swale topography is formed. This study can be referencial to agricutural and live stock production and the selection of village location.

关 键 词：清西陵 倒石堆 泥石流 地质特征 

分 类 号：P642.23[天文地球—工程地质学]