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THREE-DIMENSIONAL FINITE-DIFFERENCE MODELING OF GROUND MOTIONS IN BEIJING FROM A MW7 SCENARIO EARTHQUAKE

机译:MW7场景地震北京地面运动的三维有限差异型号

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A three-dimensional velocity model in Beijing area is constructed. The model comprises four main velocity layers. A Mw7 scenario on the Shunyi-Qianmen-Liangxiang fault is simulated. The bi-lateral and uni-lateral slip source models are used. The ground velocities are predicted using both source models. As contrast, a flat layer velocity model is constructed by averaging the depth of each layer. By doing so, the amplification factors are calculated to examine the basin effect in Beijing. The results show that, although the source models are different, the amplification factors in the Beijing basin are as high as 1.5 to 2.0.
机译:构建了北京地区的三维速度模型。该模型包括四个主速度层。模拟了顺义 - 千代 - 梁乡故障的MW7场景。使用双横向和单侧滑动源模型。使用两个源模型预测地面速度。作为对比度,通过平均每层的深度来构造平面速度模型。通过这样做,计算放大因素以检查北京的盆地效果。结果表明,虽然源模型不同,但北京盆地的放大因子高达1.5至2.0。

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