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首页> 外文期刊>Acta geodynamica et geomaterialia >Registrations of seismic foci under mining coal seam - The Experience of Polish mines
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Registrations of seismic foci under mining coal seam - The Experience of Polish mines

机译:煤矿层下地震震源的登记-波兰矿山的经验

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摘要

In the article the results of registering seismic events located under mining coal seam are presented. Such mining tremors have occurred in several Polish mines. The geological and mining conditions affecting the induction of that type of seismic events are shown. The mechanisms of deep seismic events (more than 1000m) triggered by mining are discussed in relation to regional geology. The most deep mining seismic events in Upper Silesia were related to regional geological structures focusing stress (e.g. syncline) or tectonic structures (younger faults), where mining stresses were only additional factor to trigger strong regional seismic events. The tremors were characterized by a shear mechanism in the source (double-couple forces). Tremors located directly under the performed operation, usually characterized by an uniaxial tension mechanism, associated with the regional tension axis and the space created during the operation of the coal seam, causing pushing loaded rock-mass into new gobs. Proposed methods of seismic monitoring for case of seismic events location under mining coal seam are discussed.
机译:本文介绍了记录煤层下地震事件的结果。在波兰的几座矿山中发生了这种采矿震颤。显示了影响该类型地震事件诱发的地质和采矿条件。讨论了由采矿引发的深部地震事件(大于1000m)的机理,并与区域地质有关。上西里西亚最深的采矿地震事件与集中应力(例如向斜线)或构造构造(年轻断裂)的区域地质结构有关,其中采矿应力只是触发强烈的区域地震事件的附加因素。震颤的特征在于震源的剪切机制(双耦合力)。直接在所进行的作业之下的震颤,通常以单轴张力机制为特征,与区域张力轴和煤层在作业过程中产生的空间有关,从而将加载的岩体推入新的矿块中。讨论了针对煤矿井下地震事件定位的地震监测方法。

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