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Evaluation of Seismic Potential in a Longwall Mine with Massive Sandstone Roof Under Deep Overburden

机译:深层覆膜下大规模砂岩屋顶的长壁矿地震潜力评价

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Geological factors and mine design contribute to mining-induced seismic activity, and this is especially true in longwall mining. Massive rock units are a key cause of seismic activity due to catastrophic failures that release large amounts of energy. Other factors, such as overburden depth, panel design, pillar design, rock strength, and proximity of the massive rock unit to the coal seam, all have a role in the potential and size of a seismic event. A recent seismic event was recorded by a deep longwall mine in Virginia at 3.7M_L on the local magnitude scale and 3.4 MMS by the United States Geological Survey (USGS) in July 2016, which had no impact on the mining operations. Further investigations by NIOSH and Coronado Coal researchers have shown that this event was associated with geological features that have also been associated with other, similar seismic events in Virginia. Detailed mapping and geological exploration in the mining area has made it possible to forecast possible locations for future seismic activity. In order to use the geology as a forecaster of mining-induced seismic events and the energy potential, two primary components are needed. The first component is a long history of recorded seismic events with accurately plotted locations. The second component is a high density of geologic data within the mining area. In this case, 181 events of 1.0M_Lor greater were recorded by the mine's seismic network between January, 2009, and October, 2016. Within the mining area, 897 geophysical logs were analyzed from gas wells, 224 core holes were drilled and logged, and 1,031 fiberscope holes were examined by mine geologists. From this information, it was found that overburden thickness, sandstone thickness, and sandstone quality contributed greatly to seismic locations. After analyzing the data, a pattern became apparent indicating that the majority of seismic events occurred under specific conditions. Three maps were created using MineScape geological mapping software. MineScape deploys an interpolator known as FEM (finite element method) and is based on a series of gridded triangles to forecast the probability and magnitude of an event if a particular panel were to be mined. The forecast maps have shown accuracy of within 74%-89% when compared to the recorded 181 events that were 1.0 M_L or greater when considering three major geological criteria of overburden thickness of 1900 feet or greater, 20 to 40 feet of sandstone within 50 feet of the Pocahontas number 3 seam, and a longwall caving height of 15 feet or less.
机译:地质因素和矿山设计有助于采矿诱导的地震活动,这在长墙矿业中尤其如此。由于灾难性的失败,巨大的岩石单位是遭受大量能量的灾难性失败的关键原因。其他因素,如覆盖深度,面板设计,支柱设计,岩石强度和大规模岩石单元的岩石缝,均具有震动事件的潜力和大小的作用。最近的地震事件是由弗吉尼亚州的深层长壁矿在弗吉尼亚州的一个深浪矿,2016年7月的地质调查(USGS)在局部幅度规模和3.4米姆斯,对采矿业务没有影响。 Niosh和Coronado煤矿研究人员的进一步调查表明,该事件与弗吉尼亚州其他类似地震事件的地质特征有关。采矿区的详细绘图和地质勘探使得可以预测未来地震活动的可能位置。为了使用地质,作为预测的采矿诱导的地震事件和能源潜力,需要两个主要成分。第一组件是具有精确绘制位置的记录地震事件的历史悠久。第二组分是矿区内的高密度的地质数据。在这种情况下,181名1.0M_lor的事件由2016年1月,2006年1月至10月之间的矿山地震网络记录。在矿区,897个地球物理原木从煤气井分析,钻探并记录了224枚核心孔,矿井地质学家检查了1,031个纤维孔洞。从这些信息来看,发现覆盖层厚度,砂岩厚度和砂岩质量大大贡献了地震地区。在分析数据后,模式变得明显,表明大多数地震事件发生在特定条件下。使用MINESCAPE地质映射软件创建三张地图。 MINESCAPE部署称为FEM(有限元方法)的内插器,并且基于一系列网格三角形,以预测事件的概率和幅度,如果要开采特定面板。与记录的181个事件相比,预测地图的准确性在74%-89%之内,当考虑到覆盖厚度为1900英尺或更大的三个主要地质标准时,在覆盖层厚度为1900英尺或更大的三个主要地质标准,在50英尺范围内的砂岩20至40英尺Pocahontas编号3缝,长壁塌陷高度为15英尺或更小。

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