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Long-Period Displacement Spectra of Near-Fault Strong-Motion from Tremendous Earthquakes

机译:巨大地震的近断层运动的长期位移光谱

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The characteristics of near-fault ground motion displacements, with the obvious directivity, were analyzed. Along moving direction of the fault, displacements take on the feature of fling-step, and the large pulse is the main characteristic of displacements in the vertical moving direction of the fault. The models of near-fault ground motion with different detailed scales can be obtained by median filtering with different window length on the velocity series. Displacement spectra of the models were compared with observations from tremendous earthquakes. The results show that the highly simplified model can predict the response spectrum in very long periods, but there are distinct errors in the period range in which engineering is interested (T_p < 20 sec), and the displacement spectrum of refined model is consonant with the actual spectrum in long-period (T_p > 5 sec). The refined model is necessary for very large magnitude earthquakes which include multiple rupture, and should be established according to characteristics of velocity.
机译:分析了近端故障地面运动位的特点,具有明显的方向性。沿着故障移动方向,位移采用闪烁步骤的特征,大脉冲是故障垂直移动方向上位移的主要特性。具有不同详细尺度的近故障地面运动的模型可以通过速度序列上的不同窗口长度的中值过滤获得。将模型的位移光谱与来自巨大地震的观察结果进行比较。结果表明,高度简化的模型可以在很长一段时间内预测响应频谱,但是在工程感兴趣的时间范围内存在明显的误差(T_P <20秒),并且细化模型的位移谱是辅音的辅音谱长期的实际光谱(T_P> 5秒)。精细模型对于非常大的幅度地震是必要的,其包括多次破裂,并且应根据速度的特征建立。

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