IMHE OpenIR  > 成都山地所知识仓储(2009年以前)
泥石流碎屑岩粘泥粒特征的分析研究——以云南东川蒋家沟泥石流为例
Alternative TitleANALYSIS RESEARCH ON MUDDY CLASTIC ROCK CHARACTERISTICS OF DEBRIS FLOW
Language中文
王裕宜1; 严壁玉2
Source Publication泥石流观测与研究
Editor杜榕桓 主编
Pages51-56
1996-06
Publisher科学出版社
Publication Place北京
Keyword泥石流 碎屑岩 粘泥粒
AbstractMuddy clastic rock in original area of debris flow is as a result of being uncler way of series physical and chemical actions between clastic rock under structural stress and water. They have formed an elastic - plastic - viscous textral clispersive system with high moisture , lower unit weight , ancl weak strength. lt plays an important part in formation and movement of frequent viscous debris flows.
Other Abstract泥石流形成区碎屑岩的泥粒,实质上是在构造运动作用下的碎屑岩与水相互进行一系列物理化学作用的结果。它形成了一种含水高、容重低、强度弱的弹帖塑性结构分散体系.这种分散体对于高频率粘性泥石流的形成和运动起着重要的作用.
ISBN7-03-005334-6
Document Type专著章节文集论文
Identifierhttp://ir.imde.ac.cn/handle/131551/27126
Collection成都山地所知识仓储(2009年以前)
Affiliation1.中国科学院水利部成都山地灾害与环境研究所;
2.铁道部第二勘测设计院科研所
Recommended Citation
GB/T 7714
王裕宜,严壁玉. 泥石流碎屑岩粘泥粒特征的分析研究——以云南东川蒋家沟泥石流为例. 泥石流观测与研究. 北京:科学出版社,1996:51-56.
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