摘要
该文根据汾河上游段的地层岩性 ,地貌特征、地质构造、汾河地文期及水文地质条件等资料分析了山西万家寨引黄工程南干线汾河天然河道输水段左岸滑坡群的成因和特征 ,并论证其对左岸岸坡稳定的影响。
Based on the data of stratigraphy and lithology, geomorphological characteristics, geological structure, Fenhe physiographic period, hydrogeological conditions etc. of the upstream section of Fenhe river, the paper analyzes the genesis and characteristics of the left bank landslide group of the Fenghe natural river course water conveyance section of the Huanghe river conduction project south main line in Shanxi Wanjiazhai.Also, its influences on the stability of the left bank slopes have been expounded and proved.
出处
《勘察科学技术》
2000年第4期13-16,共4页
Site Investigation Science and Technology
关键词
汾河
天然河道输水段
滑波群
地文期
引黄工程
Fenhe natural river course water conveyance section
landslide group
physiographic period
belt of weak rocks
