The packet receiver function verifies the accuracy of CRCs in the incoming packets.
报文接收功能在收到报文的时候会校验其CRC值的正确性。
Using the method of receiver function the S-wave velocity structure under Gansu seismic network is studied.
利用接收函数方法对甘肃测震台网下方的一维s波速度进行了研究。
The deep structure characteristics are inferred from the receiver function inversion with the teleseismic records in the paper.
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。
As an example, we investigate the S-wave velocity structure beneath HIA station by using the SV-component receiver function inversion method.
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。
The synthetic tests show that the convergence of SV-component receiver function inversion is faster than that of the radial receiver function inversion.
理论数值实验显示：在反演地壳S波速度结构时，SV分量接收函数比径向接收函数具有更好的收敛性。
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.
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。
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.
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。
Finally, we demonstrate application of the BPD receiver function (BPRF) method to a field dataset from Kutch, India, where near‐surface sedimentary layers are known to be present.
最后，我们陈述了将BPD接收函数方法（BPRF）应用于印度卡奇的场数据集，这里已知存在近地表沉积层。
Finally, we demonstrate application of the BPD receiver function (BPRF) method to a field dataset from Kutch, India, where near‐surface sedimentary layers are known to be present.
最后，我们陈述了将BPD接收函数方法（BPRF）应用于印度卡奇的场数据集，这里已知存在近地表沉积层。
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