Author:
Roegiers J.-C.,Thompson J. C.,McLennan J. D.
Abstract
During the extension of the Hamilton Mountain trunk sewer, instantaneous and long-term movements were monitored in the rock strata containing the excavated trench. Movements as far as 150 m from the trench axis were observed over a period of more than 1 year.Although the movements seem to be continuous and decreasing with time, their spatial distribution and dissipation are not entirely predictable, suggesting the important role of local geological features.Interpretations of the results and recommendations for other work in the region are submitted.
Publisher
Canadian Science Publishing
Subject
Civil and Structural Engineering,Geotechnical Engineering and Engineering Geology
Cited by
3 articles.
订阅此论文施引文献
订阅此论文施引文献，注册后可以免费订阅5篇论文的施引文献，订阅后可以查看论文全部施引文献