The crust in western China is in the state of isostasy.
西部地壳处于地壳均衡状态。
;The crust in western China is in the state of isostasy.
西部地壳处于地壳均衡状态。
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。
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