使用匹配滤波检测的东田纳西地震带(ETSZ) 15年的地震活动目录

Clara Daniels , Zhigang Peng
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引用次数: 1

摘要

我们提供了2005年1月1日至2020年7月31日田纳西州东部地震带(ETSZ)13671次地震的详细目录。我们对超过15年的连续数据应用了匹配滤波器检测技术,从而得出了ETSZ迄今为止最完整的地震活动目录。通过使用主成分拟合计算检测和模板之间的幅度比来确定新检测到的事件的幅度。我们还计算了新目录的b值,并使用XCORLOC和hypoDD对新检测到的事件的子集进行了比较重新定位,这显示了深度上更明确的结构。我们发现,根据磁异常的定义,纽约-阿拉巴马线沿线和以东的浓度最大,这支持了这一特征可能与ETSZ地震活动的产生有关的论点。我们检查了Watts Bar水库附近的地震活动,该水库位于约5​距离2018年12月12日田纳西州迪凯特4.4级地震震中公里,并发现该地区水库调节地震活动的可能证据。我们还研究了整个ETSZ的地震活动,以寻找浅层地震和季节水文变化之间的相关性。我们的研究结果表明,由于ETSZ的季节性地下水位,水文驱动的浅层地震活动的证据有限,这与之前的研究假设的大多数板内地震与水文循环动力学有关相矛盾。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
A 15-year-Long catalog of seismicity in the Eastern Tennessee Seismic Zone (ETSZ) using matched filter detection

We present a detailed catalog of 13 671 earthquakes in the Eastern Tennessee Seismic Zone (ETSZ) that spans January 1, 2005 to July 31, 2020. We apply a matched filter detection technique on over 15 years of continuous data, resulting in arguably the most complete catalog of seismicity in the ETSZ yet. The magnitudes of newly detected events are determined by computing the amplitude ratio between the detections and templates using a principal component fit. We also compute the b-value for the new catalog and comparatively relocate a subset of newly detected events using XCORLOC and hypoDD, which shows a more defined structure at depth. We find the greatest concentration along and to the east of the New York-Alabama Lineament, as defined by the magnetic anomaly, supporting the argument that this feature likely is related to the generation of seismicity in the ETSZ. We examine seismicity in the vicinity of the Watts Bar Reservoir, which is located about 5 ​km from the epicenter of the MW 4.4 December 12, 2018 Decatur, Tennessee earthquake, and find possible evidence for reservoir modulated seismicity in this region. We also examine seismicity in the entire ETSZ to search for a correlation between shallow earthquakes and seasonal hydrologic changes. Our results show limited evidence for hydrologically-driven shallow seismicity due to seasonal groundwater levels in the ETSZ, which contradicts previous studies hypothesizing that most intraplate earthquakes are associated with the dynamics of hydrologic cycles.

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