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。
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。
The S wave velocity structure is inferred from the receiver function for the crust and upper mantle of the Wudalianchi volcano area.
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