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.
我们使用记录在西南摩洛哥站的数据进行分析的远震P波和S波接收函数。
We use data recorded at stations in SW Morocco to analyse teleseismic P- and S-wave receiver functions.
与径向接收函数类似，SV分量接收函数可通过对远震体波的SV分量直接反褶积P分量获得。
Similar to radial receiver function, SV-component receiver function can be obtained by directly deconvolving the P-component from the SV-component of teleseismic recordings.
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