摘要
河北省磁县段广泛分布的上第三系中新统(N1)地层,其中强膨胀岩(土)对南水北调中线工程造成了很大影响。详细介绍了强膨胀岩(土)的宏观及微观地质结构,分析了其基本地质结构成因,以及裂隙面强度特征,并由此引起的滑坡现象,对其形成机理做了深入的分析阐述。
In Ci County, Hebei province wide distribution Miocene of Neogene (N1) formation, Which strong expansive rock (soil) had a great impact on Middle Route of South-to-North Water Transfer Project. This article details the strong expansion of rock (soil) of macro-and microgeological structures,Basic geological structure analysis of its causes and strength characteristics of fractured surface, And resulting landslide phenomena, In-depth analysis on the formation mechanism of its elaboration.
出处
《南水北调与水利科技》
CAS
CSCD
北大核心
2014年第B02期131-132,136,共3页
South-to-North Water Transfers and Water Science & Technology
基金
基金项目:国家“十二五”科技支撑计划项目(2011BAB10801)
关键词
南水北调中线工程
磁县
强膨胀岩(土)
地质结构
裂隙面强度
滑坡
Middle Route of South-to-North Water Transfer Project
Ci County
strong expansive rock (soil)
geological structure
fracturestrength of surface
landslide