Strong Motion Models for Duration and Arias Intensity for Strong Motion Records in Chile

IF 2.1 4区 工程技术 Q2 GEOCHEMISTRY & GEOPHYSICS
S. Cespedes, R. Boroschek, R. Ruiz
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引用次数: 0

Abstract

Chile presents a high seismicity and very particular characteristics due to its subductive environment and high convergence rate of the interacting plates. In this paper, ground motion models (GMM) for Arias Intensity and strong ground motion duration are developed based on recently compiled Chilean earthquakes records. The Chilean derived GMM are later compared with global and subduction models. For the duration case, two definitions are considered: significant duration and bracketed duration. Care is taken to consider newly define rupture areas for the major earthquake in the catalog, which allows to redefine the distances to be used in the analysis. The strong motion records are processed using robust techniques and standardized procedures. The model parameters are selected using a Bayesian updating method. This allows to estimate the parameters as well as their corresponding uncertainties recognizing the variability of the coefficients and of the selected model. The derived ground motion predictive model associated is validated through a residual analysis and probability distributions, obtained from the adjustment method. Additionally, for the bracketed duration analysis, a classification method based on Support Vector Machine (SVM) is used, with the aim to incorporate the records with duration of zero seconds. The comparison of the resultant model with the existing ones allows to confirm the differences that the tectonic Chilean environment produces, characterized mainly by a high relative convergence rate between plates and interplate thrust earthquakes with high magnitudes.
智利强震记录持续时间和咏叹调强度的强震模式
智利由于其俯冲环境和相互作用板块的高收敛速度,呈现出高地震活动性和非常特殊的特征。本文基于近年来智利地震记录,建立了阿里亚斯烈度和强地震动持续时间的地震动模型。随后将智利导出的GMM与全球模型和俯冲模型进行了比较。对于持续时间的情况,考虑了两个定义:显著持续时间和括号持续时间。考虑到目录中新定义的大地震破裂区域,这允许重新定义分析中使用的距离。强运动记录使用稳健的技术和标准化的程序进行处理。采用贝叶斯更新方法选择模型参数。这允许估计参数以及它们相应的不确定性,认识到系数和所选模型的可变性。通过残差分析和平差法得到的概率分布,验证了相应的地震动预测模型。此外,对于括号内持续时间分析,使用基于支持向量机(SVM)的分类方法,目的是将持续时间为零秒的记录纳入其中。将所得模型与现有模型进行比较,可以确认智利构造环境产生的差异,其主要特征是板块间相对收敛率高,板块间逆冲地震震级高。
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来源期刊
Journal of Earthquake and Tsunami
Journal of Earthquake and Tsunami 地学-地球化学与地球物理
CiteScore
2.60
自引率
13.30%
发文量
38
审稿时长
>12 weeks
期刊介绍: Journal of Earthquake and Tsunami provides a common forum for scientists and engineers working in the areas of earthquakes and tsunamis to communicate and interact with one another and thereby enhance the opportunities for such cross-fertilization of ideas. The Journal publishes original papers pertaining to state-of-the-art research and development in Geological and Seismological Setting; Ground Motion, Site and Building Response; Tsunami Generation, Propagation, Damage and Mitigation, as well as Education and Risk Management following an earthquake or a tsunami. We welcome papers in the following categories: Geological and Seismological Aspects Tectonics: (Geology - earth processes) Fault processes and earthquake generation: seismology (earthquake processes) Earthquake wave propagation: geophysics Remote sensing Earthquake Engineering Geotechnical hazards and response Effects on buildings and structures Risk analysis and management Retrofitting and remediation Education and awareness Material Behaviour Soil Reinforced concrete Steel Tsunamis Tsunamigenic sources Tsunami propagation: Physical oceanography Run-up and damage: wave hydraulics.
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