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Research on Microseismic Monitoring Techniques Based on Amplitude Stacking

机译:基于振幅叠加的微震监测技术研究

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Because of the complexity of the propagation path and high attenuation near the ground surface, during the process of micro-seismic monitoring, compared with the down well monitoring, the information obtained by the ground monitoring contains lower signal to noise ratio, fewer micro seismic events, and therefore poorer intepretation reliability. Amplitude stacking algorithm proposed in this paper does not need to search directly for the micro seismic events in the field data. It improves the signal to noise ratio by stacking data from all the geophones and uses reverse-time migration algorithm to locate the seismic source. Finally, we performed a forward modeling to obtain simulated 3D seismic data to prove the feasibility of the method. The seismic sources obtained by this algorithm match those defined in the synthetic model quite well. This paper provides a new algorithm for the location of micro seismic sources.
机译:由于传播路径的复杂性和地表附近的高衰减,在微地震监测过程中,与井下监测相比,地面监测获得的信息信噪比更低,微地震事件更少。 ,因此解释可靠性较差。本文提出的幅度叠加算法不需要直接在现场数据中搜索微地震事件。它通过堆叠所有地震检波器的数据来提高信噪比,并使用反向时间偏移算法来定位地震源。最后,我们进行了正向建模以获得模拟的3D地震数据,以证明该方法的可行性。通过该算法获得的地震源与合成模型中定义的地震源非常匹配。本文为微震源定位提供了一种新的算法。

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