IMHE OpenIR  > 成都山地所知识仓储(2009年以前)
浅论易滑地层
Alternative TitleDISCUSSION ON SLIDE-PRONE STRATUM
卢螽槱
Corresponding Author卢螽槱
1988
Source Publication山地研究
ISSN1008-2786
Volume6Issue:2Pages:119-122
Abstract我国不少滑坡研究者已使用过“易滑地层”一词。本文试图概述一下易滑地层及其某些特性。
Other AbstractA lot of landslide facts express that the distribution of landslide has a direct bearing on lithologic characters, i. e. the landslides are mainly distributed in some regions of stratum emergence.The strata related to the landslide are overburden and bedrock. The former is covered on the latter. The bedrock is slide-prone, so the overburien is slide-prone caused by the character of the bedrock. In nature, the overburden slide is more than bedrock. This shown that the overburden is more slide-prone than the bedrock. The slide-prone stratum, that is stratum prone to landslide, includes overburden and bedrock. It should be the essential conditions for development and activity of landslide.Some characteristics of slide-prone stratum are. i. lithologic characters are mostly sticky clay, mud stone and shale, 2. clay mineral is very rich in the slide-prone strataj 3. the shearing strength is very weak. 
Keyword集中分布 地层岩性 滑坡研究 实际资料 滑坡分布 覆盖层 滑动面 地质图 硬质岩 昔格达组
Language中文
Document Type期刊论文
Identifierhttp://ir.imde.ac.cn/handle/131551/7181
Collection成都山地所知识仓储(2009年以前)
Affiliation中国科学院成都地理研究所
First Author Affilication中国科学院水利部成都山地灾害与环境研究所
Recommended Citation
GB/T 7714
卢螽槱. 浅论易滑地层[J]. 山地研究,1988,6(2):119-122.
APA 卢螽槱.(1988).浅论易滑地层.山地研究,6(2),119-122.
MLA 卢螽槱."浅论易滑地层".山地研究 6.2(1988):119-122.
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