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链子崖T11—T12缝段危岩体开裂变形机制

MECHANISMS OF DEFORMING-CRACKING ON THE SEGMENT OF CRACKS T11-T12 OF LIANZICLIFF DANGEROUS ROCK BODY

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【作者】 刘传正张明霞

【Author】 Liu Chuanzheng;Zhang Mingxia (Institute of Environmental Geology, MGMR, Beijing. 100081)

【机构】 地质矿产部环境地质研究所

【摘要】 文章全面描述了链子崖T(11)—T(12)缝段危岩体的开裂形变特征,探讨了危岩体形成的影响因素,如重力、煤层采空区、降雨、水库蓄水、勘探掘进和地震等,指出其破坏机理是重力主导下的不对称的压力拱与悬臂梁(板)弯矩的联合作用。危岩体可以分成具有不同稳定程度的若干块体,治理工程也应针对它们的不同特点而设计。

【Abstract】 This paper is described main characteristics of deforming-cracking on the segment of cracks T(11)-T(12) of Lianzi cliff dangerous rock body, discussed a series of factors,such as gravity. coal mined-out area. rainfall, reservoir storing, exploring or driving andearthquakes on forming the dangerous rock body: its destructive mechanism is recognizedin the non-symmetry stress distribution in an arched shape of east-west direction and flexing moments of cantilever beam (plate) are induced by gravity of rock body and coalmined-out area. The dangerous rock body can be devided into a few parts, and anchoringengineering has to be designed to fit the features of these parts respectively.

  • 【文献出处】 地学前缘 ,EARTH SCIENCE FRONTIERS , 编辑部邮箱 ,1996年02期
  • 【分类号】P583
  • 【被引频次】13
  • 【下载频次】110
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