KMS Institute of Mountain Hazards and Environment,CAS
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. |
Files in This Item: | ||||||
File Name/Size | DocType | Version | Access | License | ||
64-66.pdf(418KB) | 专著章节文集论文 | 开放获取 | CC BY-NC-SA | View Application Full Text |
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