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Seismic and geotechnical investigations following a rockburst in a complex French mining district

机译:法国一个复杂矿区的岩爆后的地震和岩土勘察

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摘要

This paper presents the results of seismic and geotechnical studies carried out after a fatal accident that occurred during mining of the Frieda5 coal seam at Merlebach mine of HBL (Houilleres du Bassin Lorrain, East France). On June 21, 2001, a violent rockburst (local magnitude of 3.6) affected the Frieda5 seam at depth of approximately 1250 m. The zone of the accident-is located in the main gate 200 m ahead of the longwall face. Subsequently, an investigation was carried out to determine the causes of the accident and to understand the induced phenomenon. The program included an analysis of a comprehensive set of seismic data and the collection of in-situ stress measurements. The objectives were twofold: (1) to provide input data for the back analysis of the rockburst and (2) to identify other potential high-risk zones in the next panels to be mined. The joint analysis of the seismic, geological and geotechnical investigations suggests that the rockburst is largely due to a specific geological phenomenon, a sandstone channel in the floor of the coal seam characterized by high horizontal stresses.
机译:本文介绍了在HBL Merlebach矿(Houilleres du Bassin Lorrain,法国东部)的Frieda5煤层开采期间发生的致命事故之后进行的地震和岩土工程研究的结果。 2001年6月21日,剧烈的岩爆(局部震级为3.6)影响了Frieda5煤层,深度约为1250 m。事故区域位于长壁前面200 m的主闸门中。随后,进行了调查以确定事故原因并了解引起的现象。该计划包括对一套完整的地震数据进行分析,并收集现场应力测量值。目标是双重的:(1)为岩爆的反分析提供输入数据,(2)在接下来要开采的面板中识别其他潜在的高风险区域。地震,地质和岩土工程研究的联合分析表明,岩爆主要是由于特定的地质现象所致,即煤层底板上的砂岩通道具有高水平应力。

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