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Spatial variation in stress in seismogenic zones in South African gold mines

机译:南非金矿地震区应力的空间变化

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We review our endeavor to probe spatial variation in stress in seismogenic zones in deep hard-rock gold mines in South Africa. Highly stressed ground, especially in remnants or pillars, often increases the risks posed by normal-faulting earthquakes to mining operations. Some of these seismogenic zones were identified by AE monitoring, allowing us to explore them with drill holes shorter than several tens of meters in length. A M5.5 strike-slip earthquake, not a usual mining-induced earthquake, took place in 2014 on an unknown nearly-vertical geological structure, with the upper fringe of the aftershock zone several hundreds of meters below the mining horizons. The aftershock zone was elucidated by in-mine dense geophone network and surface strong motion network. This allowed us to drill two holes of 817 and 700 m length from 2.9 km depth. Integration of in-situ stress measurements by both conventional and new methods allows us to constrain the stress field accurately.
机译:我们致力于努力探测南非深层硬岩金矿中的地区原子区压力的空间变化。高度紧张的地面,特别是在残余或柱子中,通常会增加正常断层地震到采矿业务所带来的风险。通过AE监测鉴定了一些这些发酵区域,允许我们探索它们的钻孔,短于几十米的长度。一个M5.5滑动地震,而不是一种通常的采矿地震,于2014年在未知的几乎垂直的地质结构上发生,余震区域上部边缘几百米以下的矿区。通过矿井茂密的地震孔网络和表面强运动网络阐明了余震区。这允许我们从2.9公里深度钻出817和700米长的两个孔。通过常规和新方法的原位应力测量的集成允许我们准确地限制应力场。

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