首页> 外文期刊>Journal of geophysical research. Solid earth: JGR >Cross Validation of Stress Drop Estimates and Interpretations for the 2011 Prague, OK, Earthquake Sequence Using Multiple Methods
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Cross Validation of Stress Drop Estimates and Interpretations for the 2011 Prague, OK, Earthquake Sequence Using Multiple Methods

机译:使用多种方法交叉验证压力下降估算和2011年,OK,地震序列的解释

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We compare source parameter estimates for earthquakes in the 2011 Prague Mw 5.7, Oklahoma, sequence to investigate random uncertainty and systematic bias, and resolve reliable relative variations in stress drop. Source parameters provide insight into the earthquake rupture processes but large variations between studies occur. The Prague earthquake sequence is a prime example of this, with different studies reaching contrasting interpretations of the effects of injection on source parameters. We examine the Prague earthquake sequence using a single coherent catalog for all the events detected by the Oklahoma Geological Survey (OGS) and McMahon et al. (2017). We use three principal approaches to estimate stress drop in order to understand the biases of each: a spectral decomposition method based on stacking, individual event spectral modeling, and a spectral ratio method based on highly correlated events. We also compare our results with previous studies for the Prague sequences aftershocks, as well as past results for the Mw 4.8 foreshock and Mw 4.8 aftershock and Mw 5.7 mainshock. The absolute values of stress drop vary significantly between methods, but the relative patterns remain consistent, except when low quality or low bandwidth data are included. The consistent relative patterns reveal that the stress drops of aftershocks are dependent on the fault orientation and the proximity of the events to the mainshocks slip. These results indicate that fault structure as well as past events play an important role in stress drop patterns.
机译:我们比较了2011年俄克拉何马州布拉格5.7兆瓦地震序列的震源参数估计,以调查随机不确定性和系统偏差,并解决应力降的可靠相对变化。震源参数提供了对地震破裂过程的洞察,但研究之间存在很大差异。布拉格地震序列就是一个很好的例子,不同的研究得出了注入对震源参数影响的对比解释。我们使用俄克拉何马州地质调查局(OGS)和麦克马洪等人(2017)检测到的所有事件的单一相干目录来检查布拉格地震序列。我们使用三种主要方法来估计应力降,以了解每种方法的偏差:基于叠加的谱分解方法、单个事件谱建模和基于高度相关事件的谱比方法。我们还将我们的结果与之前对布拉格序列余震的研究以及过去对兆瓦4.8级前震、兆瓦4.8级余震和兆瓦5.7级主震的结果进行了比较。应力降的绝对值在不同方法之间存在显著差异,但相对模式保持一致,除非包含低质量或低带宽数据。一致的相对模式表明,余震的应力降取决于断层方向和事件与主震滑动的距离。这些结果表明,断层结构和过去的事件在应力降模式中起着重要作用。

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