基于近几年GPS测量的研究结果，提出利用GPS实测应变率对岩石圈流变结构进行约束的新方法。
We present a new constraint on the rheological structure of the lithosphere whose strain rate obtained from GPS data.
方法通过岩石圈温度结构约束，计算了岩石圈流变学结构。
Methods lithospheric rheological structure has been inverted by lithospheric temperature structure constraint.
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