{"title":"An EGF technique to infer the source parameters of a circular crack growing at a variable rupture velocity","authors":"Salvatore de Lorenzo, Maddalena Michele","doi":"10.3389/feart.2024.1428167","DOIUrl":null,"url":null,"abstract":"Circular crack models with a constant rupture velocity struggle to effectively model both the amplitude and duration of first P-wave pulses generated by small magnitude seismic events. Assuming a constant rupture velocity is unphysical, necessitating a deceleration phase in the rupture velocity to uphold the causality of the healing process. Moreover, a comprehensive failure model might encompass an initial nucleation phase, typically characterized by an increase of the initial rupture velocity. Studies have demonstrated that quasi-dynamic circular crack models featuring variable rupture velocities can accurately model the shape of the observed first P-wave pulse. Based on these principles, an Empirical Green’s function (EGF) approach was previously formulated to estimate the source parameters of small magnitude earthquakes, called MAIN. In addition to determine the source radius and stress drop, this method also enables the inference of the temporal evolution of rupture velocity. However, this method encounters difficulties when the noise-to-signal ratio in the recordings of smaller earthquakes used as EGF exceeds 5%, a common situation when employing regional-scale recordings of small-magnitude earthquakes as EGF. Through synthetic tests, we demonstrated that, in such instances, the problem of this technique is that the alignment between the onset of P waves of EGF and MAIN is not rightly recovered after the initial inversion step. Consequently, a novel inversion method has been developed to address this issue, enabling the identification of the optimal alignment of P-wave arrivals in EGF and MAIN across all stations. A Bayesian statistical approach is proposed to meticulously investigate the solutions of model parameters and their correlations. Using the new technique on a small magnitude earthquake (ML = 3.3) occurred in Central Italy enabled us to identify the most likely rupture models and examine the issue of correlation among model parameters. Application of Occam’s Razor Principle suggests that, for the investigated event, a circular crack model should be favored over a heterogeneous rupture model.","PeriodicalId":505744,"journal":{"name":"Frontiers in Earth Science","volume":"91 3","pages":""},"PeriodicalIF":0.0000,"publicationDate":"2024-07-16","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Frontiers in Earth Science","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.3389/feart.2024.1428167","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0
Abstract
Circular crack models with a constant rupture velocity struggle to effectively model both the amplitude and duration of first P-wave pulses generated by small magnitude seismic events. Assuming a constant rupture velocity is unphysical, necessitating a deceleration phase in the rupture velocity to uphold the causality of the healing process. Moreover, a comprehensive failure model might encompass an initial nucleation phase, typically characterized by an increase of the initial rupture velocity. Studies have demonstrated that quasi-dynamic circular crack models featuring variable rupture velocities can accurately model the shape of the observed first P-wave pulse. Based on these principles, an Empirical Green’s function (EGF) approach was previously formulated to estimate the source parameters of small magnitude earthquakes, called MAIN. In addition to determine the source radius and stress drop, this method also enables the inference of the temporal evolution of rupture velocity. However, this method encounters difficulties when the noise-to-signal ratio in the recordings of smaller earthquakes used as EGF exceeds 5%, a common situation when employing regional-scale recordings of small-magnitude earthquakes as EGF. Through synthetic tests, we demonstrated that, in such instances, the problem of this technique is that the alignment between the onset of P waves of EGF and MAIN is not rightly recovered after the initial inversion step. Consequently, a novel inversion method has been developed to address this issue, enabling the identification of the optimal alignment of P-wave arrivals in EGF and MAIN across all stations. A Bayesian statistical approach is proposed to meticulously investigate the solutions of model parameters and their correlations. Using the new technique on a small magnitude earthquake (ML = 3.3) occurred in Central Italy enabled us to identify the most likely rupture models and examine the issue of correlation among model parameters. Application of Occam’s Razor Principle suggests that, for the investigated event, a circular crack model should be favored over a heterogeneous rupture model.
具有恒定破裂速度的圆形裂缝模型难以有效模拟小震级地震事件产生的第一 P 波脉冲的振幅和持续时间。假设恒定的破裂速度是不符合实际情况的,这就需要在破裂速度上有一个减速阶段,以维护愈合过程的因果关系。此外,一个全面的故障模型可能包含一个初始成核阶段,其典型特征是初始破裂速度的增加。研究表明,以可变断裂速度为特征的准动态圆形裂缝模型可以准确模拟观察到的第一个 P 波脉冲的形状。根据这些原理,以前制定了一种经验格林函数(EGF)方法来估计小震级地震的震源参数,称为 MAIN。除了确定震源半径和应力降之外,这种方法还能推断断裂速度的时间演变。然而,当用作 EGF 的较小地震记录的噪声信号比超过 5%(这是使用区域尺度小震记录作为 EGF 时的常见情况)时,该方法就会遇到困难。通过合成测试,我们证明了在这种情况下,该技术的问题是在初始反演步骤之后,EGF P 波的起始点与 MAIN 之间的排列无法正确恢复。因此,我们开发了一种新的反演方法来解决这一问题,从而能够确定所有站点的 EGF 和 MAIN P 波到达的最佳排列。提出了一种贝叶斯统计方法,以仔细研究模型参数及其相关性的解决方案。在意大利中部发生的一次小震级地震(ML = 3.3)中使用新技术,使我们能够确定最有可能的破裂模型,并研究模型参数之间的相关性问题。奥卡姆剃刀原理的应用表明,对于所研究的事件,圆形裂缝模型应优于异质破裂模型。