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Using the Morris sensitivity analysis method to assess the importance of input variables on time-reversal imaging of seismic sources

机译:利用MORRIS敏感性分析方法评估输入变量对地震源的时间逆转成像的重要性

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The time-reversal imaging method has become a standard technique for seismic source location using both acoustic and elastic wave equations. Although there are many studies on the determination of the relevant parameter for visualization of the time-reversal method, little has been done so far to investigate the accuracy of seismic source location depending on parameters such as the geometry of the seismic network or underestimation of the velocity model. This paper investigates the importance of the accuracy of seismic source location using the time-reversal imaging method of input variables such as seismic network geometry and the assumed geological model. For efficient visualization of seismic wave propagation and interference, peak-to-average power ratio was used. Identification of the importance of variables used in seismic source location was obtained using the Morris elementary effect method, which is a global sensitivity analysis method.
机译:时间反转成像方法已成为使用声学和弹性波形方程的地震源位置的标准技术。尽管有很多关于确定用于可视化的相关参数的研究,但到目前为止,迄今为止已经研究了根据地震网络的几何形状的参数来研究地震源位置的准确性或低估速度模型。本文研究了使用输入变量的时转成像方法等地震源位置的准确性的重要性,如地震网络几何和假设的地质模型。为了有效可视化地震波传播和干扰,使用峰平均功率比。使用Morris基本效应方法获得识别地震源位置中使用的变量的重要性,这是一种全局敏感性分析方法。

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