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Study of the Rock Mass Failure Process and Mechanisms During the Transformation from Open-Pit to Underground Mining Based on Microseismic Monitoring

机译:基于微震监测的露天矿区转化岩体破坏过程及机制研究

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摘要

To quantitatively understand the failure process and failure mechanism of a rock mass during the transformation from open-pit mining to underground mining, the Shirengou Iron Mine was selected as an engineering project case study. The study area was determined using the rock mass basic quality classification method and the kinematic analysis method. Based on the analysis of the variations in apparent stress and apparent volume over time, the rock mass failure process was analyzed. According to the recent research on the temporal and spatial change of microseismic events in location, energy, apparent stress, and displacement, the migration characteristics of rock mass damage were studied. A hybrid moment tensor inversion method was used to determine the rock mass fracture source mechanisms, the fracture orientations, and fracture scales. The fracture area can be divided into three zones: Zone A, Zone B, and Zone C. A statistical analysis of the orientation information of the fracture planes orientations was carried out, and four dominant fracture planes were obtained. Finally, the slip tendency analysis method was employed, and the unstable fracture planes were obtained. The results show: (1) The microseismic monitoring and hybrid moment tensor analysis can effectively analyze the failure process and failure mechanism of rock mass, (2) during the transformation from open-pit to underground mining, the failure type of rock mass is mainly shear failure and the tensile failure is mostly concentrated in the roof of goafs, and (3) the rock mass of the pit bottom and the upper of goaf No. 18 have the possibility of further damage.
机译:为了定量地了解岩石在露天挖掘到地下采矿过程中岩石的故障过程和失效机制,石油古铁矿被选为工程项目案例研究。使用岩体碱性质量分类方法和运动分析方法测定研究区域。基于分析表观应力和表观量随时间的表观体积的变化,分析了岩体输出失效过程。根据近期对位置,能量,表观应力和位移的微震事件的时间和空间变化的研究,研究了岩体质量损伤的迁移特性。混合动力片刻张量反转方法用于确定岩体骨折源机构,断裂取向和裂缝尺度。裂缝区域可分为三个区域:区域A,区域B和区域C.进行了断裂平面取向的取向信息的统计分析,并获得了四个显性裂缝。最后,采用滑动趋势分析方法,得到不稳定的断裂架。结果表明:(1)微震监测和混合动力片刻张量分析可以有效分析岩体的故障过程和故障机制,(2)在露天坑转换到地下采矿过程中,故障类型的岩体主要是主要的剪切失效和拉伸衰竭大多集中在公羊屋顶上,(3)坑底部的岩石质量和GOF的上部有可能进一步损坏。

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