The crust in western China is in the state of isostasy.
中国西部地壳处于地壳衡状态。
The crust in western China is in the state of isostasy.
中国西部地壳处于地壳衡状态。
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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