isostasy

基本解释

Some classical models of isostasy are discussed.
讨论了一些有关地壳均衡概念的模型。
The crust in western China is in the state of isostasy.
中国西部地壳处于地壳均衡状态。
A new model of isostasy is introduced corresponding to a certain rotational regime of the earth.
介绍一种新的地壳均衡模型，它与地球的某一种旋转方式相适应。
Based on isostasy principle, this paper made out a correction method for the calculation of disconformity erosion amount.
考虑地壳均衡效应，可以对传统的地层剥蚀量计算方法进一步修正。
The last stage occurred in Late Cenozoic time (ca. 5Ma), dominated by differential uplift, caused by extension and isostasy due to change in climate.
第4阶段始于晚新生代（5百万年），以差异性隆升为特征，其中，点苍山的隆升是构造成因，而哀牢山山体的形成可能与红河的下切相辅相成，有限的隆升是地壳发生均衡反弹造成的。