摘要
本文对阳安线新渔坝古错落体的基本特征作了阐述 ,并探讨了该错落体的变形演变过程及形成机理 ,在此基础上提出了同类地区的工作方法及建议。
The paper expounds the basic characteristics of the Xinyuba ancient scattered earth-body in Yangpingguan-Ankang Railway Line. It explores also the evolution procedure of its deformation and the formation mechanism of this scattered earth-body. Based on these conceptions, the methods and suggestions are proposed for works at the similar regions.
出处
《铁道工程学报》
EI
2003年第1期104-107,103,共5页
Journal of Railway Engineering Society
