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Analysis on Deformation and Failure Process of Wangxia Dangerous Rock Pillar W1

机译:王霞危险岩柱W1变形破坏过程分析

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摘要

The dynamic deformation process of Wangxia dangerous rock pillar W1 is studied on the basis of geological survey and field monitoring.The dangerous rock, located in Liangping Town of Wushan County in Chongqing, was cut into cylinder shapes by fissures.The lithology of the dangerous rock body is thick layer siliceous argillaceous limestone with flint, while the lithology of its foundation bed is siltstone, clay rock and seam, which forms a rigid upper layer and soft lower layer structure.The results indicates that the displacement deformation curve of the dangerous rock pillar can be divided into four stages, including early accumulated deformation, uniform deformation, accelerated deformation and critical accelerated deformation.The special geologic structure and environment provides a geologic base for the deformation and failure of dangerous rock pillars.And the effect of human activities and rainfall is conspicuous.
机译:在地质调查和野外监测的基础上,研究了望厦危险岩柱W1的动态变形过程,将位于重庆市巫山县梁坪镇的危险岩通过裂隙切割成圆柱状。主体为厚层的硅质灰质灰质灰岩,其基床的岩性为粉砂岩,粘土岩和煤层,形成了刚性的上层和软的下层结构。结果表明,危险岩柱的位移变形曲线可以分为早期累积变形,均匀变形,加速变形和临界加速变形四个阶段。特殊的地质构造和环境为危险岩柱的变形和破坏以及人类活动和降雨的影响提供了地质基础。很明显。

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