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Determination of intraplate focal mechanisms with the Brazilian Seismic Network: A simplified Cut-and-Paste approach

机译:利用巴西地震台网确定板内焦点机制:一种简化的剪切和粘贴方法

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? 2022 Elsevier LtdThe feasibility of a simplified Cut-and-Paste approach (CAP) for routine determination of intraplate earthquake mechanisms in Brazil is demonstrated with data acquired by the Brazilian Seismographic Network (RSBR). Our approach models three-component seismic recordings through: (i) computation of synthetics seismograms with a single, average velocity model, and (ii) independent alignment of observed and synthetic waveforms through waveform cross-correlation. No partitioning of regional waveforms into their corresponding body- and surface-wave trains is considered. The empirical alignment successfully accounts for lateral variations along specific source-station paths, along with location uncertainties and timing errors, and effectively augments the number of waveforms available for inversion. The performance of the proposed approach is demonstrated through modeling of two recent intraplate earthquakes: the Mw 4.4 2017 Maranh?o earthquake and the Mw 4.1 2020 Amargosa earthquake. For the Maranh?o event, we obtain a strike-slip focal mechanism (340° ± 0°, 70° ± 0°, 0° ± 0°) and a centroid depth of 9 km with magnitude of Mw 4.4, fully consistent with previous studies. For the Amargosa earthquake, we obtain a normal-fault mechanism (20° ± 4.6°, 60° ± 16.9°, -30° ± 14.4°) with a preferred centroid depth of 10 km, which is in general agreement with P-wave polarity data and the orientation of the nearby Salvador Shear Zone. We thus conclude that our simplified CAP approach is an effective tool for modeling regional waveforms in Brazil and, most likely, in sparse networks in general.
机译:?2022 年,爱思唯尔有限公司巴西地震台面网络 (RSBR) 获取的数据证明了简化的剪切和粘贴方法 (CAP) 在巴西常规测定板块内地震机制的可行性。我们的方法通过以下方式对三分量地震记录进行建模:(i) 使用单一的平均速度模型计算合成地震图,以及 (ii) 通过波形互相关对准观测波形和合成波形的独立对齐。没有考虑将区域波形划分为相应的体波和表面波序列。经验对准成功地解释了沿特定源站路径的横向变化,以及位置不确定性和定时误差,并有效地增加了可用于反演的波形数量。通过对最近的两次板块内地震进行建模,证明了所提出的方法的性能:2017年Mw 4.4 Maranh?o地震和2020年Mw 4.1 Amargosa地震。对于Maranh?o事件,我们获得了走滑焦点机制(340°±0°,70°±0°,0°±0°),质心深度为9 km,星等为Mw 4.4,与以前的研究完全一致。对于阿马戈萨地震,我们得到了一个正断层机制(20°±4.6°、60°±16.9°、-30°±14.4°),优选质心深度为10 km,这与P波极性数据和附近萨尔瓦多剪切带的方位基本吻合。因此,我们得出结论,我们的简化CAP方法是对巴西区域波形进行建模的有效工具,而且很可能是在一般的稀疏网络中。

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