蒋家沟泥石流源地滑坡类型初探

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 Title	PRELIMINARY 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
Pages	64-66
	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
Abstract	The 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。
ISBN	7-03-005334-6
Document Type	专著章节文集论文
Identifier	http://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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