S-wave velocity structure S波速度结构
S-wave velocity structure inversion S速度结构反演
-d s wave velocity structure 三维s波速度结构
shallow S-wave velocity structure 浅层剪切波速度结构
3-d s wave velocity structure 三维s波速度结构
The S wave velocity structure is inferred from the receiver function for the crust and upper mantle of the Wudalianchi volcano area.
可以推断，从接收器功能的S波速度结构 五大连池火山区地壳和上地幔的。
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。
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。
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