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.
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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