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A new location method of microseismic source without pre-measuring speed

机译:无需预测量速度的微震源定位新方法

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In recent decade, geophysical methods, such as microseismic monitoring, geotomography, and in-seam seismic techniques, have shown an increased significance in rock physical mechanics and mining engineering.Especially the developments of seismic monitoring bring hope to predict the rock burst and seismic hazards, where potential location determination of hypocenter is the key technology.In previous study, the location techniques all need two hypotheses: 1) The propagation speed can be measured accurately;2) Seismic wave propagates in homogeneous, isotropic geological structures.While in practical applications, heterogeneous geological structure makes the medium (what the seismic wave propagation) shows anisotropic feature instead of isotropic.Meanwhile measuring the propagation speed accurately is very difficult.In order to solve these two problems, localization method of microseismic source based on the genetic algorithm without pre-measuring speed is proposed.This method assumes that the seismic wave propagates in the direction of a spindle, and the propagation speed is the fastest along the spindle direction.The equations are established in which the source position, propagation speed and spindle orientation are variables.Finally, the equations were solved through genetic algorithm.The comparison between the predict results by our method and the experimental data measured in DongGua Copper showed that the proposed method can predict the source location more accurately, and with a good prospect.
机译:近十年来,诸如微地震监测,地貌学和煤层内地震技术等地球物理方法在岩石物理力学和采矿工程中显示出越来越重要的意义。特别是地震监测的发展为预测岩爆和地震灾害带来了希望在以前的研究中,定位技术都需要两个假设:1)可以精确测量传播速度; 2)地震波在均质各向同性的地质结构中传播。异质的地质结构使得介质(地震波的传播)呈现出各向异性而不是各向同性的特征,同时准确地测量传播速度是非常困难的。为解决这两个问题,基于遗传算法的微震源定位方法没有提出了预测量速度。该方法假定地震波沿主轴方向传播,沿主轴方向传播速度最快,建立了震源位置,传播速度和主轴方位为变量的方程式,最后通过遗传算法求解通过我们方法的预测结果与在东瓜铜矿中测得的实验数据的比较表明,该方法可以更准确地预测震源位置,具有良好的前景。

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