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首页> 外文期刊>International Journal of Rock Mechanics and Mining Sciences >In situ monitoring and analysis of the mining-induced deep ground movement in a metal mine
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In situ monitoring and analysis of the mining-induced deep ground movement in a metal mine

机译:原位监测与分析金属矿井挖掘诱导的深地运动

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An extra-deep multiple-point borehole extensometer, applicable up to 300 m depth of cover, is introduced for the deformation monitoring of the deep rock masses (i.e., the rock mass below the ground surface) in the eastern area of Jinshandian Iron-ore Mine, and the in situ monitoring results collected over eight years are analysed. Combined with the deformation monitoring results on the ground surface collected by using a Global Positioning System (GPS), Level Monitoring Technique, and a three-dimensional Laser Scanning System (Leica HDS 880), the ground movement mechanism of the deep rock masses induced by underground mining is investigated. Results show that the extra-deep multiple-point borehole extensometer can capture the deformation information pertaining to deep rock masses in metal mines with complex geological conditions such as Jinshandian Iron-ore Mine. The moment that the deformation of the monitoring point starts to increase significantly can be used to determine whether the major deformation has transferred to the deep rock mass at the monitoring points, or not: the monitoring results from such critical moments indicate that the major deformation of the overburden strata gradually develops from the lower part to the upper part, consistent with the results from a physical modelling experiment. In Jingshandian Iron-ore Mine, the second caving of the deep rock masses reaches the ground surface above the centre of the mined-out area, and then causes the ground collapse; under the combined effect of the underground mining in Jinshandian Iron-ore Mine and the remaining private mined-out areas, large-scale ground surface collapses and cracks can be observed in mining-affected areas. The deep rock masses surrounding the mined-out areas are in a state of global deformation, and the boundary line of the deep break zone is a fold line. Currently, the rock masses in the major deformation zone move downwards under gravity on the shear surfaces in Jingshandian Iron-ore Mine.
机译:适用于高达300米的盖子的深层多点钻孔扩展仪,引入了金斯坦伊铁 - 矿石东部地区深层岩石(即,地面下方岩石质量)的变形监测矿山,分析了超过八年的原位监测结果。结合通过使用全球定位系统(GPS),水平监测技术和三维激光扫描系统(Leica HDS 880)收集的地表上的变形监测结果,深层岩体诱导的深层移动机构调查地下采矿。结果表明,深层多点钻孔伸展计可以捕获金属地矿深层岩石群体的变形信息,具有复杂的地质条件,如金斯迪亚铁矿石矿。监测点的变形变形的那一刻,可以用于确定主要变形是否转移到监测点处的深层岩石质量,而不是:来自这种关键时刻的监测结果表明主要变形覆盖层层从下部到上部逐渐发展,与物理建模实验的结果一致。在JingShandian的铁矿石中,深层岩石的第二个洞穴到达挖出区域中心上方的地面,然后导致地面塌陷;在金斯迪亚铁矿石矿山地下采矿的综合效应下,在采矿地区可以观察到大型地表坍塌和裂缝。覆盖区域周围的深层岩体处于全球变形状态,深度断裂区的边界线是折叠线。目前,主要变形区中的岩石块在jingshandian铁矿矿的剪切表面上的重力下向下移动。

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