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首页> 外文期刊>Bulletin of earthquake engineering >Empirical ground-motion models for point- and extended-source crustal earthquake scenarios in Europe and the Middle East
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Empirical ground-motion models for point- and extended-source crustal earthquake scenarios in Europe and the Middle East

机译:欧洲和中东点源和扩展源地壳地震场景的经验地面运动模型

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This article presents the latest generation of ground-motion models for the prediction of elastic response (pseudo-) spectral accelerations, as well as peak ground acceleration and velocity, derived using pan-European databases. The models present a number of novelties with respect to previous generations of models (Ambraseys et al. in Earthq Eng Struct Dyn 25:371-400, 1996, Bull Earthq Eng 3:1-53, 2005; Bommer et al. in Bull Earthq Eng 1:171- 203, 2003; Akkar and Bommer in Seismol Res Lett 81:195-206, 2010), namely: inclusion of a nonlinear site amplification function that is a function of VS30 and reference peak ground acceleration on rock; extension of the magnitude range of applicability of the model down to Mw 4; extension of the distance range of applicability out to 200km; extension to shorter and longer periods (down to 0.01 s and up to 4 s); and consistent models for both point-source (epicentral, Repi, and hypocentral distance, Rhyp) and finite-fault (distance to the surface projection of the rupture, RJB) distance metrics. In addition, data from more than 1.5 times as many earthquakes, compared to previous pan-European models, have been used, leading to regressions based on approximately twice as many records in total. The metadata of these records have been carefully compiled and reappraised in recent European projects. These improvements lead to more robust ground-motion prediction equations than have previously been published for shallow (focal depths less than 30km) crustal earthquakes in Europe and theMiddle East.We conclude with suggestions for the application of the equations to seismic hazard assessments in Europe and the Middle East within a logic-tree framework to capture epistemic uncertainty.
机译:本文介绍了最新一代的地面运动模型,用于预测使用泛欧洲数据库得出的弹性响应(伪)谱加速度以及峰值地面加速度和速度。与前几代模型相比,这些模型具有许多新颖性(Ambraseys等人在Earthq Eng Struct Dyn 25:371-400,1996,Bull Earthq Eng 3:1-53,2005; Bommer等人在Bull Earthq中Eng 1:171-203,2003; Akkar和Bommer在Seismol Res Lett 81:195-206,2010中),即:包含一个非线性站点放大函数,该函数是VS30和岩石上参考峰值地面加速度的函数;将模型的适用幅度范围扩大到Mw 4;适用距离范围扩大到200km;延长至较短和较长的时间(低至0.01 s至4 s);以及点源(显性,Repi和下中心距,Rhyp)和有限断层(到破裂表面投影的距离,RJB)距离度量的一致模型。此外,与以前的泛欧洲模型相比,已经使用了超过1.5倍地震的数据,从而导致基于总数大约两倍的记录进行回归。这些记录的元数据已在最近的欧洲项目中进行了仔细的编辑和重新评估。与欧洲和中东的浅层地震(震源深度小于30 km)地壳地震预测公式相比,这些改进导致了更健壮的地面运动预测方程式。最后,我们建议将该方程式应用于欧洲和中东的地震危险性评估中逻辑树框架中的中东来捕获认知不确定性。

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