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论层状基岩斜坡的变形特征和临滑判据
Alternative TitleDEFORMABILITY CHARACTISTIC AND SLIDING CRITERION OF THE DIP SLOPE IN STRATIFIED ROCK MASSES
Language中文
吴其伟
1989-10
Source Publication一九八七年全国滑坡学术讨论会滑坡论文选集
Author of Source《滑坡论文选集》编辑委员会 ; 中国科学院成都山地灾害与环境研究所
Pages148-152
meeting一九八七年全国滑坡学术讨论会
Conference Date1987-10-21~25
Conference Place成都
Country中国
Publication Place成都
Publisher四川科学技术出版社
Contribution Rank1
Abstract在我国西南,广泛分布着由砂泥岩组成的层状结构基岩岸坡,大型滑坡经常在这类基岩斜坡中发生。文中对同向缓倾层状基岩斜坡的变形特征、临滑判据和稳定性分析等进行了研究。根据调查研究的结果,提出了这类大型基岩滑坡的成因机制和讨论它的临滑判据问题。
Other AbstractIn the Southwest of China, there exists wildely a kind of rock slope of bedded structure which consists of sandstone and mudstone. The huge landslide is of freauent occurrence in this kind of rock slope. In this paper, the dip slope of this kind is studied in the three cased:(1) deformability characteristic; (2) failling condition; (3) stability analysis.
According to these investigation and study results the forming-mechanism of huge rock landslide is presented and discussed it's sliding driterion.
Keyword滑坡 斜坡
Subject Area岩土力学 ; 工程地质学 ; 灾害学
ISBN7-5361594-X
Indexed By其他
Document Type会议论文
Identifierhttp://ir.imde.ac.cn/handle/131551/26588
Collection成都山地所知识仓储(2009年以前)
Corresponding Author吴其伟
Affiliation中国科学院成都山地灾害与环境研究所
First Author Affilication中国科学院水利部成都山地灾害与环境研究所
Corresponding Author Affilication中国科学院水利部成都山地灾害与环境研究所
Recommended Citation
GB/T 7714
吴其伟. 论层状基岩斜坡的变形特征和临滑判据[C]//《滑坡论文选集》编辑委员会, 中国科学院成都山地灾害与环境研究所. 成都:四川科学技术出版社,1989:148-152.
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