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A Stochastic Method for Investigating Site Effects by Means of a Borehole Array—SH and Love Waves

机译:通过钻孔阵列(SH和爱波)研究场地效应的随机方法

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摘要

A stochastic method for investigating site effects by means of borehole array observation is proposed. This method is based on a stochastic time-series model that is derived from Haskell's matrix procedure for a layered medium and is applicable to transverse-component recordings simultaneously obtained on the ground surface and at a depth. The time-series model not only accounts for the amplitude but also for the phase characteristics of the recordings. By applying this method to actual downhole array recordings, the following aspects of site effects can be investigated: (1) An estimation of the wave transfer function for SH waves, (2) the separation of upcoming and downgoing waves on a borehole seismogram at a depth, that is, an estimation of purely incident waves, and (3) the enhancement of fundamental mode Love eaves on a surface seismogram are examined by applying this method to two borehole array recordings obtained at the Fuchu observatory in Japan. A noteworthy point is that these aspects of site effects are examined using this method without any knowledge of the velocity structure beneath the site.
机译:提出了一种通过井眼阵列观测研究场地效应的随机方法。该方法基于随机时间序列模型,该模型是从Haskell的矩阵方法对层状介质进行推导的,适用于同时在地面和深度获得的横向分量记录。时间序列模型不仅考虑幅度,而且考虑记录的相位特性。通过将该方法应用于实际的井下阵列记录,可以研究以下方面的现场影响:(1)估算SH波的波传递函数,(2)在井眼地震图上分离出即将到来的和向下的波通过将这种方法应用于在日本府中天文台获得的两个井眼阵列记录中,研究了深度,即纯入射波的估计以及(3)地表地震波基本爱模式的增强。值得注意的一点是,在不了解场地下方速度结构的情况下,使用此方法检查了场地效果的这些方面。

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