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COHERENCY FUNCTION MODEL OF GROUND MOTIONAT BASE-ROCK

机译:地基基岩的相干函数模型

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At present, the method to study spatial variation of ground motions is statistic analysis based on densearray records such as SMART-1 array, etc, to get coherency function of ground motion, which would beused to depict the variation with space and frequency. But there is no coherency function model of baserock.In this paper, spatial variation of stochastic ground motions at base-rock, which considering thefactors of rupture velocity, numbers of sub-source, depth of epicenter and propagation velocity, is studiedfrom near-field ground motions which are simulated by elastic half-space model with dislocation source offault. In the case of lack of statistic coherency function of base-rock, the results of this paper are usefuland could be referenced.
机译:目前,研究地震动空间变化的方法是基于诸如SMART-1阵列等密集阵列记录的统计分析,以获得地震动的相干函数,用于描述地震动的空间和频率变化。但是没有基岩的相干函数模型。本文从近场研究了破裂速度,子源数,震中深度和传播速度等因素对基岩随机地震动的空间影响。地震动是通过弹性半空间模型对位错源进攻进行模拟的。在缺乏基岩统计相关函数的情况下,本文的研究结果是有用的,可为参考。

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