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首页> 外文期刊>Journal of Earthquake Engineering >A Fast and Efficient Simulation of the Far-Fault and Near-Fault Earthquake Ground Motions Associated with the June 17 and 21, 2000, Earthquakes in South Iceland
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A Fast and Efficient Simulation of the Far-Fault and Near-Fault Earthquake Ground Motions Associated with the June 17 and 21, 2000, Earthquakes in South Iceland

机译:快速有效地模拟与2000年6月17日至21日在南冰岛发生的地震有关的远断层和近断层地震

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摘要

The two M_w 6.5 earthquakes on June 17 and 21, 2000, respectively, in the populated South Iceland Seismic Zone (SISZ) significantly augmented the Icelandic database of strong ground motions, and several strong velocity pulses were recorded at near-fault sites. The strong motions are interpreted via the Specific Barrier Model (SBM) and a mathematical model of near-fault velocity pulses. The data indicates self-similar source scaling and significantly greater attenuation of seismic waves than in other interplate regions. Through inversion of the data a new attenuation function for the SISZ has been adopted, which results in unbiased simulations. For the first time, the characteristics of the recorded near-fault pulses have been identified and compared to the worldwide database of such records. The SBM and the near-fault pulse model combine naturally in a fast and efficient synthesis of realistic, broad-band strong ground motions in the far-fault and near-fault region. Such simulations are showcased for the June 2000 earthquakes and indicate that the modeling approach adopted in this study is an effective tool for the estimation of realistic earthquake ground motions in the SISZ.
机译:2000年6月17日和21日分别在人口密集的南冰岛地震区(SISZ)发生的两次M_w 6.5级地震大大增强了冰岛有关强地面运动的数据库,并且在近断层现场记录了几个强速度脉冲。强运动通过特殊屏障模型(SBM)和接近故障速度脉冲的数学模型进行解释。数据表明自相似的震源尺度和比其他板间区域明显更大的地震波衰减。通过数据反演,采用了SISZ的新衰减函数,从而实现了无偏仿真。首次识别出所记录的近故障脉冲的特征,并将其与此类记录的全球数据库进行比较。 SBM和近断层脉冲模型自然地组合在一起,可以快速有效地合成远断层和近断层区域中现实的,宽带的强地面运动。对2000年6月地震进行了此类模拟,表明该研究采用的建模方法是估算SISZ中实际地震地面运动的有效工具。

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