成都大学学报（自然科学版）2025，Vol.44Issue(2)：211-217,7.DOI:10.3969/j.issn.1004-5422.2025.02.014
S207线沱江沿岸某滑坡成因机制及稳定性研究
Study on Formation Mechanism and Stability of a Landslide along Tuojiang River on S207 Line
王龙1
作者信息
- 1. 四川省交通勘察设计研究院有限公司,四川成都 610017
- 折叠
摘要
Abstract
The S207 line from Fushun Anxi to Zhaohua,located along parallel ridges and valleys of eastern Sichuan,is adjacent to the east of Tuojiang River and close to the west of steep slopes.The expansion of the leading edge road will cause a series of landslide problems.This paper takes a typical landslide in this section as an example.Through field geological mapping,field visits,supplemented by geological drilling,and consulting regional geological background information,the engineering geological conditions and gene-sis mechanism of the landslide are identified.The stability of the landslide is calculated and analyzed,and treatment suggestions for specific purposes are proposed.This study provides a geological basis for the ex-pansion and engineering treatment of the province-level road in this section,and also provides a certain reference for the treatment of the landslide occurring in the anticline folded mountain in parallel ridges and valleys in eastern Sichuan.关键词
沱江/滑坡/成因机制/稳定性/背斜Key words
Tuojiang River/landslide/formation mechanism/stability/anticline分类
交通运输引用本文复制引用
王龙..S207线沱江沿岸某滑坡成因机制及稳定性研究[J].成都大学学报（自然科学版）,2025,44(2):211-217,7.
