Terra nova. 1991;3(4):393-400. doi: 10.1111/j.1365-3121.1991.tb00168.x Q31.92025

The present rate of uplift of Fennoscandia implies a low-viscosity asthenosphere

芬诺斯堪的亚目前的抬升速率表明其软流圈具有低黏度。

DOI: 10.1111/j.1365-3121.1991.tb00168.x

摘要

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