从尾声信封中提取的英国 MW 目录

Charlie Peach, S. Nippress, David N Green, Kevin Mayeda, James M Wookey, M. J. Werner
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摘要

英国(UK)的地震活动处于中低水平;在过去 20 年中,仅记录了 12 次局部震级(ML)≥ 4.0 的陆上地震。因此,使用常规矩张量反演法很难估算出英国大部分地震的矩震级 (MW),导致对 MW 的可靠估算有限。为了解决这个问题,我们对分布在英国各地的 16 个宽带地震台站的尾音包络进行了校准,为 2006 年以来发生的 100 次矩幅≥2.13 的事件编制了矩幅目录。这需要使用开源的 Coda 校正工具,该工具需要独立的震源参数估计来进行校准。对于 2006 年至 2022 年间英国发生的 13 次事件,我们使用频谱建模估算视应力(0.32 至 1.74 兆帕),并使用矩张量反演估算兆瓦(3.35 至 4.52)。这些独立的震源参数构成了最终校准输入的一个子集,最终校准使用了来自 33 个事件的地震数据,校准值为 2.57 (le $Mw$ (le $4.49)。由此得出的尾波校准参数被应用于另外 67 个事件(MW≥2.13)。整个英国的尾音包络表现出缓慢的地震尾音衰减,在 20 Hz 以下有明显的能量,这与其他构造活动较少的地区是一致的。该 MW 目录以及对未来英国地震事件的校准应用将有助于评估地震危害和事件特征。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
A UK MW catalogue derived from coda envelopes
The United Kingdom (UK) experiences low-to-moderate levels of seismicity; only 12 onshore earthquakes with local magnitude (ML) ≥ 4.0 have been recorded in the past 20 years. It is therefore difficult to estimate moment magnitude (MW) using conventional moment tensor inversion for the majority of UK seismicity, resulting in limited reliable estimates of MW. To address this, we calibrated coda envelopes at 16 broadband seismic stations distributed across the UK, to produce a MW catalogue for 100 events with MW≥2.13 that occurred since 2006. This was achieved using the open-source Coda Calibration Tool, which requires independent source parameter estimates for calibration. For 13 UK events between 2006 and 2022, we used spectral modelling to estimate apparent stress (0.32 to 1.74 MPa), and moment tensor inversion to estimate MW (3.35 to 4.52). These independent source parameters formed a subset of the inputs into the final calibration, which used seismic data from 33 events with coda-derived values of 2.57$\le $Mw$\le $4.49. The resultant coda calibration parameters were applied to 67 further events (MW≥2.13). The coda envelopes exhibit slow seismic coda decay across the UK, with significant energy up to 20 Hz, consistent with other regions of low tectonic activity. This MW catalogue, and the application of the calibration to future UK seismic events, will be useful for both assessing seismic hazard and event characterisation.
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