Asthenosphere uplift indicates the deep adjustment process during the interaction of plates, and also shows the adjusting process of gravitational equilibrium between upper layer of crust and mantle.

软流圈隆升是板块相互作用的深部调整过程，同时也是地壳表层—地幔进行重力均衡调整的过程。

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Earlier projections apparently failed to account for rebounding changes in the Earth's crust following the last Ice Age (referred to as "glacial isostatic adjustment").

FORBES: Magazine Article