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A preliminary empirical model for frequency-dependent attenuation of Fourier amplitude spectra In Serbia from the Vrancea earthquakes

机译:弗朗塞地震中塞尔维亚傅立叶振幅谱衰减随频率而变的初步经验模型

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We present the frequency-dependent attenuation model for Fourier amplitude spectra of strong earthquake ground motion in Serbia from intermediate depth earthquakes in the Vrancea source zone in Romania. The development of this type of scaling is the essential first step toward developing the corresponding attenuation and scaling equations for pseudo relative velocity spectra (PSV), which are necessary for seismic macro- and microzoning in the territory of Serbia. Such scaling is necessary because the Vrancea source zone produces large earthquakes with shaking that attenuates differently from the local earthquakes in Serbia. Development of such a scaling model is associated with several difficulties, the principal one being the lack of recorded strong motion accelerograms at epicentral distances exceeding 300 km. To reduce uncertainties with such scaling, we require our preliminary scaling equations to be consistent with independent estimates of seismic moment, stress drop, and radiated wave energy. In the future, when the recorded strong motion data from Vrancea earthquakes increases several-fold of what it is today, it will become possible to perform this analysis again, thus leading to more reliable and permanent scaling estimates. (C) 2015 Elsevier Ltd. All rights reserved.
机译:我们提出了罗马尼亚Vrancea震源区中深度地震中塞尔维亚强烈地震地面运动的傅立叶振幅谱的频率依赖衰减模型。开发这种类型的缩放比例是朝拟定伪相对速度谱(PSV)的相应衰减和缩放比例方程式迈出的重要第一步,这对于塞尔维亚境内的地震宏观和微观分区是必不可少的。之所以需要这样的缩放比例,是因为Vrancea震源区产生的大地震带有震荡,其衰减不同于塞尔维亚当地的地震。这种缩放模型的开发与若干困难有关,主要的困难是在震中距离超过300 km时缺少记录的强运动加速度图。为了减少这种缩放的不确定性,我们要求我们的初步缩放方程与地震矩,应力降和辐射波能量的独立估计一致。将来,当记录的来自Vrancea地震的强运动数据增加到今天的几倍时,将有可能再次执行此分析,从而获得更可靠和永久的缩放估计。 (C)2015 Elsevier Ltd.保留所有权利。

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