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Picking versus stacking in a modern microearthquake location: Comparison of results from a surface passive seismic monitoring array in Oklahoma

机译:现代微震地点的拾取与叠加:俄克拉荷马州地表被动地震监测阵列的结果比较

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We present location results for a group of similar to 200 microearthquakes that occurred in 2012 in a region of Oklahoma hosting ongoing exploration activities. Using a local passive surface seismic monitoring network of 15 broadband stations, we applied two modern location techniques that use fundamentally different approaches. The first is a pick-based double-difference relocation method with waveform crosscorrelation. Multiple-event location techniques such as these are generally regarded as the best approach for obtaining high-precision locations from pick data. The second approach is an automated waveform migration stacking method. These types of methods are becoming increasingly common due to increasing network station density and computer power. The results from the two methods show excellent agreement and provide similar results for the interpreter. Both methods reveal spatial and temporal patterns in the locations that are not visible in results obtained using a more traditional pick-based approach. We performed two statistical uncertainty tests to assess the effects of data quality and quantity on the two methods. We show that the uncertainties for both methods are comparable, but that the stack-based locations are less sensitive to station geometry, likely due to the different treatment of outliers and the beneficial inclusion of noisier data. Finally, we discuss the favorable conditions in which to apply each method and argue that for small aperture surface arrays where accurate velocity information exists, such as in this study, the stack-based method is preferable due to the higher degree of automation. Under these conditions, stack-based methods better allow for rapid and precise determination of microearthquake locations, facilitating improved interpretations of seismogenic processes.
机译:我们提供了2012年在俄克拉荷马州进行中的持续勘探活动的一组类似的200次微地震的定位结果。通过使用由15个宽带站组成的本地无源地面地震监测网络,我们应用了两种使用根本不同方法的现代定位技术。第一种是具有波形互相关的基于拾取的双差分重定位方法。诸如此类的多事件定位技术通常被认为是从拾取数据中获取高精度位置的最佳方法。第二种方法是自动波形迁移堆叠方法。由于网络站密度和计算机功率的增加,这些类型的方法变得越来越普遍。两种方法的结果显示出极好的一致性,并为口译员提供了相似的结果。两种方法都揭示了在使用更传统的基于拾取方法获得的结果中不可见的位置中的空间和时间模式。我们执行了两个统计不确定性测试,以评估数据质量和数量对这两种方法的影响。我们显示两种方法的不确定性是可比较的,但是基于堆栈的位置对站点几何不太敏感,这可能是由于对异常值的不同处理以及对噪声数据的有益考虑。最后,我们讨论了应用每种方法的有利条件,并指出对于存在准确速度信息的小孔径表面阵列,例如本研究中,由于较高的自动化程度,基于堆栈的方法是可取的。在这种情况下,基于堆栈的方法更好地实现了对微震位置的快速,准确的确定,从而有助于改进对震源过程的解释。

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