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Simultaneous inversion of multiple microseismic data for event locations and velocity model with Bayesian inference

机译:与贝叶斯推断的事件位置和速度模型同时反演多微观型数据

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We have applied Bayesian inference for simultaneous inversion of multiple microseismic data to obtain event locations along with the subsurface velocity model. The traditional method of using a predetermined velocity model for event location may be subject to large uncertainties, particularly if the prior velocity model is poor. Our study indicated that microseismic data can help to construct the velocity model, which is usually a major source of uncertainty in microseismic event locations. The simultaneous inversion eliminates the requirement for an accurate predetermined velocity model in microseismic event location estimation. We estimate the posterior probability density of the velocity model and microseismic event locations with the maximum a posteriori estimation, and the posterior covariance approximation under the Gaussian assumption. This provides an efficient and effective way to quantify the uncertainty of the microseismic location estimation and capture the correlation between the velocity model and microseismic event locations. We have developed successful applications on both synthetic examples and real data from the Newberry enhanced geothermal system. Comparisons with location results based on a traditional predetermined velocity model method demonstrated that we can construct a reliable effective velocity model using only microseismic data and determine microseismic event locations without prior knowledge of the velocity model.
机译:我们已经应用了贝叶斯推断,同时反演多种微震数据,以便与地下速度模型一起获得事件位置。使用用于事件位置的预定速度模型的传统方法可能受到大的不确定性,特别是如果先前的速度模型差。我们的研究表明,微震数据可以有助于构建速度模型,这通常是微震事件位置中不确定性的主要来源。同时反演消除了微震事件位置估计中精确的预定速度模型的要求。我们估计具有最大后验估计的速度模型和微震事件位置的后验概率密度,以及高斯假设下的后协方差近似。这提供了一种有效且有效的方法来量化微震定位估计的不确定性并捕获速度模型与微震事件位置之间的相关性。我们在纽伯利增强地热系统中开发了合成示例和实际数据的成功应用程序。基于传统的预定速度模型方法的位置结果的比较证明我们可以仅使用微震数据构建可靠的有效速度模型,并确定微震事件位置而无需先前了解速度模型。

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