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Rupture process of four medium-sized earthquakes that occurred in the Gulf of California

机译:加利福尼亚湾发生的四次中型地震的破裂过程

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Four medium-sized earthquakes (M w Global CMT project 5.5, 5.6, 5.9, 6.3; hereinafter named Topolobampo, Angel de la Guarda, San Lorenzo, and Loreto earthquakes, respectively) located in the Gulf of California Extensional Province were studied to obtain their kinematic rupture processes. A network of broadband seismic stations located around the Gulf of California recorded the events (Network of Autonomously Recording Seismographs–Baja and Red Sísmica de Banda Ancha). Inversion of the seismic moment tensor and body waveform modeling were used to obtain the fault geometry and slip distribution on the fault plane, respectively. From these analyses, we obtained source depths of the order of 5.5 ± 0.5 km. We found also that the source rupture processes of the Topolobampo and Angel de la Guarda events have simple moment rate functions and source time durations of 5.0 ± 1.2 and 4.2 ± 1.2 s, respectively. The Topolobampo event was a right-lateral strike-slip event, and Angel de la Guarda was a normal event. The San Lorenzo and Loreto shocks show a rather complex rupture, with source time durations of 7.5 ± 1.2 and 9.0 ± 1.2 s, respectively. For these earthquakes, we tested the resolution of numerical results, performing an extra inversion with smoother waveforms. The new inversions do not show the separated patches of slip, as in the first analysis, but the slip distribution has an elongated shape not characteristic of simple events. We cannot therefore conclude rupture propagation for the San Lorenzo event, although the extent of the patch for the Loreto earthquake agrees with aftershock locations. Estimates of source time durations for these earthquakes are at the upper limit of the values found for earthquakes elsewhere. Directions of P axes are in the same order of magnitude as the maximum horizontal stress obtained for the so-called Gulf of California stress province from borehole elongations, focal plane solutions, and fault slip data.
机译:研究了位于加利福尼亚延伸省海湾的四次中级地震(Mw Global CMT项目5.5、5.6、5.9、6.3;以下分别称为Topolobampo,Angel de la Guarda,San Lorenzo和Loreto地震),以获取地震资料。运动破裂过程。位于加利福尼亚湾周围的宽带地震台站网络记录了该事件(自主记录地震仪网络-Baja和RedSísmicade Banda Ancha)。利用地震矩张量的反演和人体波形建模分别获得了断层平面上的断层几何特征和滑动分布。从这些分析中,我们获得了5.5±0.5 km量级的震源深度。我们还发现Topolobampo事件和Angel de la Guarda事件的震源破裂过程具有简单的矩速率函数,震源持续时间分别为5.0±1.2和4.2±1.2 s。 Topolobampo事件是右侧走滑事件,Angel de la Guarda事件是正常事件。 San Lorenzo和Loreto震荡显示出相当复杂的破裂,震源持续时间分别为7.5±1.2和9.0±1.2 s。对于这些地震,我们测试了数值结果的分辨率,并使用更平滑的波形执行了额外的反演。新的反演没有像第一个分析那样显示滑移的分离斑块,但是滑移分布具有细长的形状,不是简单事件的特征。因此,尽管洛雷托地震的斑块程度与余震位置一致,但我们不能就圣洛伦佐事件的破裂传播得出结论。这些地震的震源持续时间的估计值是在其他地方发现的地震值的上限。 P轴的方向与从井眼延伸率,焦平面解和断层滑动数据获得的所谓的加利福尼亚湾应力省的最大水平应力的数量级相同。

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