首页> 外文OA文献 >Hybrid Broadband Ground-Motion Simulations: Combining Long-Period Deterministic Synthetics with High-Frequency Multiple S-to-S Backscattering
【2h】

Hybrid Broadband Ground-Motion Simulations: Combining Long-Period Deterministic Synthetics with High-Frequency Multiple S-to-S Backscattering

机译:混合宽带地面运动模拟:将长期确定性合成与高频多重S-S反向散射相结合

代理获取
本网站仅为用户提供外文OA文献查询和代理获取服务,本网站没有原文。下单后我们将采用程序或人工为您竭诚获取高质量的原文,但由于OA文献来源多样且变更频繁,仍可能出现获取不到、文献不完整或与标题不符等情况,如果获取不到我们将提供退款服务。请知悉。

摘要

We present a new approach for computing broadband (0-10 Hz) synthetic seismograms by combining high-frequency (HF) scattering with low-frequency (LF) deterministic seismograms, considering finite-fault earthquake rupture models embedded in 3D earth structure. Site-specific HF-scattering Green's functions for a heterogeneous medium with uniformly distributed random isotropic scatterers are convolved with a source-time function that characterizes the temporal evolution of the rupture process. These scatterograms are then reconciled with the LF-deterministic waveforms using a frequency-domain optimization to match both amplitude and phase spectra around the target intersection frequency. The scattering parameters of the medium, scattering attenuation ηs, intrinsic attenuation ηi, and site-kappa, as well as frequency-dependent attenuation, determine waveform and spectral character of the HF-synthetics and thus affect the hybrid broadband seismograms. Applying our methodology to the 1994 Northridge earthquake and validating against near-field recordings at 24 sites, we find that our technique provides realistic broadband waveforms and consistently reproduces LF ground-motion intensities for two independent source descriptions. The least biased results, compared to recorded strong-motion data, are obtained after applying a frequency-dependent site-amplification factor to the broadband simulations. This innovative hybrid ground-motion simulation approach, applicable to any arbitrarily complex earthquake source model, is well suited for seismic hazard analysis and ground-motion estimation.
机译:考虑到嵌入3D地球结构中的有限断层地震破裂模型,我们提出了一种通过组合高频(HF)散射与低频(LF)确定性地震图来计算宽带(0-10 Hz)综合地震图的新方法。具有均匀分布的随机各向同性散射体的异质介质的特定于站点的HF散射格林函数与表征破裂过程随时间变化的源时间函数进行卷积。然后,使用频域优化将这些散点图与LF确定性波形进行协调,以匹配目标相交频率附近的振幅和相位频谱。介质的散射参数,散射衰减ηs,固有衰减ηi和位点kappa,以及与频率相关的衰减,决定了HF合成器的波形和频谱特性,从而影响了混合宽带地震图。将我们的方法应用于1994年Northridge地震并针对24个站点的近场记录进行验证,我们发现我们的技术提供了逼真的宽带波形,并且始终如一地再现了LF地面运动强度,用于两个独立的震源描述。与频率记录的强运动数据相比,在宽带模拟中应用频率相关的站点放大系数后可获得的偏差最少。这种创新的混合地震动模拟方法适用于任何任意复杂的地震源模型,非常适合地震危险性分析和地震动估计。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
代理获取

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号