摘要
本文论述了黄石板岩山危岩体地形、地貌及地质构造特征 ,分析讨论了其成因机理 ,得出危岩体已处于蠕变后期 ,位移变形趋于稳定。不会再次发生大规模的整体倾倒破坏 ,提出了活石清理、裂缝顶部加盖排水指导的防治措施。
In this paper, geological environment and geomorphological characteristics of geological hazards on Banyanshan mountain are introduced, and formation mechanism of the hazards is discussed. It is concluded that any large geological hazard will not occur, since the dangerous rock is in the late ereep stage and deformation tends to be stable. Therefore, the most important job is to control the landslide stability.
出处
《工程地质学报》
CSCD
2000年第2期202-205,共4页
Journal of Engineering Geology
