地面被动地震监测由局部近似采用

M. J. Khoshnavaz, A. Bόna, K. Chambers, H. Siahkoohi, Alireza Khoshnavaz
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引用次数: 2

摘要

对采矿活动和水力压裂产生的被动震源进行监测,在危害分析和非常规储层开发中具有重要作用。地面阵列在此类监测场景中被广泛使用,其优势是空间监测孔径更大,因此比井下阵列监测的体积更大。然而,表面阵列记录的信噪比自然较低。这使得基于相干技术的应用成为地面监测的合适选择。在使用基于相干性的监测方法来定位被动地震事件时,与震源机制相对应的极性变化是一项复杂的任务。为了克服这个问题,我们建议采用一种直接的方法,将相似性作为一致性分析工具应用于单独的台站集群,然后对所有集群的结果进行平均。为了评估该方法的性能,我们将其应用于反斜震源生成的半合成被动地震数据示例,并将结果与基于相干的经典技术的应用结果进行了比较。结果表明,该方法能够克服极性变化任务,而无需进行任何极性校正步骤。
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Surface passive seismic monitoring by the local use of semblance
Summary Monitoring of passive seismic sources generated by mining activities and hydraulic fracturing has an important role in hazard analysis and in development of unconventional reservoirs. Surface arrays are vastly used in such monitoring scenarios with the advantage of wider spatial monitoring aperture, thus monitoring larger volumes over downhole arrays. However, signal-to-noise ratio of surface array records is naturally low. That makes application of coherency-based techniques an appropriate option for surface monitoring. Polarity variations corresponding to the source mechanism across the moveout curves/surfaces is a complicating task in the use of coherency-based monitoring methods to locate passive seismic events. To overcome this issue, we suggest a straight-forward approach that applies semblance, as a coherency analysis tool, on separate clusters of stations followed by averaging the results from all the clusters. To evaluate the performance of the suggested approach, we applied it on a semi-synthetic passive seismic data example generated from a reverse-oblique source and compared the result with the outcome from application of the classic coherency-based technique. It shows the ability of the suggested method to overcome polarity variations task, without conducting any polarity correction step.
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