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Moment tensor inversion for two micro-earthquakes occurring inside the Háje gas storage facilities, Czech Republic

机译:捷克共和国 Háje 储气设施内发生的两次微地震的矩张量反演

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摘要

Broadband data from the P?íbram seismological network was used to investigate the source of two earthquakes, with magnitudes Mw = 0. 2 and 0. 4 respectively, occurring in the period of October-November 2009 in the Háje natural gas storage area (Czech Republic). Both events were located inside the limits of the storage area and at depths similar to those of the underground caverns where the gas is stored. We applied an inversion technique using the software ISOLA for moment tensor retrieval in order to assess the source process of both events and recognize whether a significant isotropic component existed that could be interpreted as a possible cavern collapse. We also performed an uncertainty analysis so as to confirm the reliability of the focal mechanism solutions and we controlled the consistency between the inverted focal mechanisms and those calculated using the P-waves first motions. Our results showed that the nodal plane orientation, the centroid depth, and the magnitude remained stable. Furthermore, we calculated synthetic waveforms for collapse-type ruptures and compared them with the original records. The match between the synthetic and the original data was very poor supporting the interpretation of the shear character of the events. The combination of the inversion results, which indicated significant double-couple components and of the synthetic tests, which supported the inexistence of an isotropic component at the source, led to the conclusion that the possibility of rocks falling from the ceiling of the caverns or a cavern collapse is highly unlikely.
机译:来自P?íbram地震网络的宽带数据用于调查两次地震的来源,震级为Mw = 0。2 和 0。4 分别发生在2009年10月至11月期间,发生在Háje天然气储存区(捷克共和国)。这两个事件都位于储存区的范围内,其深度与储存气体的地下洞穴的深度相似。我们使用软件ISOLA应用了一种反演技术进行矩张量检索,以评估两个事件的源过程,并识别是否存在可以解释为可能的洞穴坍塌的显着各向同性分量。我们还进行了不确定性分析,以确认焦点机制解决方案的可靠性,并控制了倒置焦点机制与使用 P 波第一运动计算的焦点机制之间的一致性。结果表明,节点平面方向、质心深度和幅度保持稳定。此外,我们计算了坍塌型破裂的合成波形,并将其与原始记录进行了比较。合成数据与原始数据之间的匹配度非常差,无法解释事件的剪切特性。反演结果表明存在显著的双耦合成分,而综合测试则支持源头不存在各向同性成分,两者相结合,得出的结论是,岩石从洞穴顶部掉落或洞穴坍塌的可能性极小。

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