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Study on the Deformation Features of the Controlling Crack T10 at the Back Edge of Wangxia Dangerous Rock Area in Wushan County

机译:巫山县王霞危险岩地区后边缘控制裂纹T10变形特征研究

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In August 2010, serious deformation occurred in the Wangxia dangerous rock mass. It formed a large dangerous factor for the local resident and channel safety. Based on the detailed investigation of the crack, deformation history, GPS observations and crack displacement monitoring data analysis, analysed comprehensively the deformation of Crack T10 and relationship with the dangerous rock. The results show that Crack T10 is controlling crack and the back edge of the deformation zone. Each segment of the crack was mainly on settlement during aggravation deformation period. East and west segmentation of the crack was mainly on settlement during gentle transition period, but the tension deformation of the middle segmentation was stronger than settlement deformation. The dislocation of each segment was not obvious. This was mainly caused by the crack extension direction different from the overall deformation direction of the rear edge of the dangerous rock, and controlled by the deformation direction of the rear edge collapse pits. Crack T10 was closely associated relation with the dangerous rock mass and the deformation had bigger effect with the old cracks and mining activities at the bottom. Crack T10 also was the key area to react the dynamic deformation and failure of the dangerous rock. And also can provide efficient accurate real-time information for the warning forecast work of Wangxia dangerous rock. According to the geological conditions and the deformation character of Crack T10, think Wangxia dangerous rock is subsided extrusion type collapse.
机译:2010年8月,王峡危险岩石质量发生严重变形。它为当地居民和渠道安全形成了一个很大的危险因素。基于对裂缝,变形历史,GPS观测和裂纹位移监测数据分析的详细研究,全面分析了裂缝T10的变形及与危险岩石的关系。结果表明,裂缝T10是控制变形区的裂缝和后边缘。裂缝的每个段主要在加重变形期间沉降。裂缝的东部和西部分割主要是在温和过渡期间的沉降,但中间细分的张力变形比沉降变形更强烈。每个细分的错位并不明显。这主要是由裂缝延伸方向不同于危险岩石后边缘的整体变形方向引起的,并由后边缘塌陷坑的变形方向控制。裂缝T10与危险的岩石质量密切相关,变形与底部的旧裂缝和采矿活动更大。裂缝T10也是反应危险岩石的动态变形和失效的关键区域。并且还可以为王霞危险岩石的警告预测工作提供有效的准确实时信息。根据地质条件和裂缝T10的变形特征,认为王霞危险岩石是抗挤压型塌陷。

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