从短期来看，它们之间的关系由短期偏离向长期均衡调整的力度较大。
The adjustment degree of their relation from short-term deviation to long-term balance is big.
它是在褶皱冲断带负载的作用下，岩石圈通过区域性均衡调整及流变挠曲而形成的。
They were formed through regional isostatic adjustment and Theological flexure under the load of fold-thrust belts.
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。
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.
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