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What moved where?: The impact of velocity uncertainty on microseismic location and moment-tensor inversion

机译:什么移动到哪里?:速度不确定性对微震位置和力矩张量反演的影响

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摘要

With the rise of unconventional resources, microseismic monitoring is becoming increasingly important because of its cost-effectiveness. This has led to significant research activity on how best to locate events and characterize their moment tensors. Locations tell us where fracturing is occurring, allow the tracking of fluid movement, and fracture propagation. Moment tensors help to determine the type of failure occurring, which is beneficial in planning and interpreting the results of hydraulic-fracturing jobs and in monitoring production. The rising number of methods to determine parameters raises important questions about how uncertainties in the input parameters are translated into uncertainties in the final locations and moment tensors. We present a framework for assessing these uncertainties and use it to demonstrate how velocity uncertainty — as well as uncertainties in arrival times and amplitudes — translates into uncertainties on the recovered quantities of location and moment-tensor parameters.
机译:随着非常规资源的增加,微地震监测由于其成本效益而变得越来越重要。这导致了关于如何最佳定位事件和表征其矩张量的重大研究活动。位置告诉我们发生裂缝的位置,可以追踪流体运动和裂缝扩展。矩张量有助于确定发生的故障类型,这对计划和解释水力压裂作业的结果以及监控生产非常有利。确定参数的方法数量不断增加,提出了有关输入参数的不确定性如何转换为最终位置和力矩张量的不确定性的重要问题。我们提出了一个评估这些不确定性的框架,并用它来证明速度不确定性以及到达时间和振幅的不确定性如何转化为位置和力矩张量参数的回收量的不确定性。

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