IMHE OpenIR  > 成都山地所知识仓储(2009年以前)
蒋家沟泥石流源地滑坡类型初探
Alternative TitlePRELIMINARY STUDY OF THE LANDSLIDE TYPES IN SOURCE AREA OF DEBRIS FLOW IN JIANGJIA RAVINE
Language中文
胡发德; 田连权
Source Publication泥石流观测与研究
Editor杜榕桓 主编
Pages64-66
1996-06
Publisher科学出版社
Publication Place北京
Keyword蒋家沟 泥石流源地 滑披类型
AbstractThe formation of debris flow and the development of landslide are boullcl by a common cause. According to the observatioll alld research in Jiallgjia Ravine. it is known that the era of landslide formation and the speed of its activity determine the quantity of loose solid materials for debris flow. This paper classifies the lalldslicles by the velocity of sliding.
Other Abstract蒋家沟泥石流的形成与该沟滑坡发育过程休戚相关。我们的观测研究资料表明:由滑披形成的时代、活动的速度决定了泥石流土石体来量的多少。因而本文以滑速的不同对滑坡进行了分类。
ISBN7-03-005334-6
Document Type专著章节文集论文
Identifierhttp://ir.imde.ac.cn/handle/131551/27128
Collection成都山地所知识仓储(2009年以前)
Affiliation中国科学院东川泥石流观测研究站
Recommended Citation
GB/T 7714
胡发德,田连权. 蒋家沟泥石流源地滑坡类型初探. 泥石流观测与研究. 北京:科学出版社,1996:64-66.
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