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Waveform Inversion-Assisted Distributed Reverse Time Migration for Microseismic Location

机译:波形反演辅助分布式反向时间迁移微震位置

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摘要

We present a novel approach to locate microseismic sources in situ and in real time in distributed sensor networks (DSN). We propose a distributed reverse time migration (RTM) microseismic source location algorithm. RTM-based methods have advantages in passive source location in terms of robustness and accuracy. However, the traditional methods have a centralized data collection and ex situ postprocessing style, and were not designed for in situ and real-time seismic imaging, so communication and computation costs were not considered. Utilizing newly emerging DSN, real-time and in situ microseismic source location becomes possible. Thus, we specially design a joint imaging condition for the DSN system to reduce both computation and communication burdens. The tradeoff, however, is location resolution reduction. Sequentially, we employ a waveform inversion approach to obtain a finer resolution microseismic source location result. Finally, we validate the proposed method using both synthetic and field seismic records. Our approach shows promising performances using synthetics with single and multiple sources, as well as with field data. The proposed waveform inversion-assisted distributed RTM location algorithm obtains high-resolution source location results and significantly reduced communication and computation costs, even at a low signal-to-noise ratio.
机译:我们提出了一种新颖的方法来定位微震源原位,实时定位在分布式传感器网络(DSN)中。我们提出了一种分布式反向时间迁移(RTM)微震源定位算法。基于RTM的方法在鲁棒性和准确性方面具有被动源位置的优势。但是,传统方法具有集中式数据收集和EX原位的后处理风格,并没有设计用于原位和实时地震成像,因此不考虑通信和计算成本。利用新出现的DSN,实时和原位微震源位置成为可能。因此,我们专门设计了DSN系统的联合成像条件,以减少计算和通信负担。但是,权衡是定位分辨率降低。顺序地,我们采用波形反演方法来获得更精细的分辨率微震源位置结果。最后,我们使用合成和场地震记录验证了所提出的方法。我们的方法显示了使用具有单个和多个来源的合成和多种来源的有前途的表演,以及现场数据。即使以低信噪比,所提出的波形反转辅助分布式RTM位置算法获得了高分辨率源位置结果并显着降低了通信和计算成本。

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