远震（Far earthquake）是指发生地震时，震中距大于1000公里或10°的地震。
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提出了适合于近震及远震定位的球面交切法。
The method of spherical surface shearing suitable for the location of near and far earthquake was proposed.
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.
确实有一些证据能说明远震会增加世界其他地方后续地震发生的风险。
There is some evidence that distant earthquakes might increase the risk of subsequent quakes around the world (see 'Past quakes cause future shocks').
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