采用远震接收函数反演的方法揭示了该区域的深部结构特征。
The deep structure characteristics are inferred from the receiver function inversion with the teleseismic records in the paper.
作为实例，利用SV分量接收函数反演方法反演了海拉尔台下的S波速度结构。
As an example, we investigate the S-wave velocity structure beneath HIA station by using the SV-component receiver function inversion method.
利用唐山近场强震记录对如何分析场地反应进行研究，分析比较了多种方法：线性反演法、传统的谱比法以及接收函数法。
We compared site response from the S wave inversion and those from other techniques, such as traditional direct spectral ratios of S waves and receiver function of S waves.
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