isostasy

基本解釋

Some classical models of isostasy are discussed.
討論了一些有關(guān)地殼均衡概念的模型。
The crust in western China is in the state of isostasy.
中國西部地殼處于地殼均衡狀態(tài)。
A new model of isostasy is introduced corresponding to a certain rotational regime of the earth.
介紹一種新的地殼均衡模型，它與地球的某一種旋轉(zhuǎn)方式相適應(yīng)。
Based on isostasy principle, this paper made out a correction method for the calculation of disconformity erosion amount.
考慮地殼均衡效應(yīng)，可以對(duì)傳統(tǒng)的地層剝蝕量計(jì)算方法進(jìn)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階段始于晚新生代（5百萬年），以差異性隆升為特征，其中，點(diǎn)蒼山的隆升是構(gòu)造成因，而哀牢山山體的形成可能與紅河的下切相輔相成，有限的隆升是地殼發(fā)生均衡反彈造成的。