这些为认识用大地测量方法定量研究现代地壳变动的客观性提供了理论基础。
So the theoretical bases for objective recognizing the recent crustal movements by using the quantitative research of geodetic method are supplied by means of this study.
尤其是四千多年前那次地壳变动引来的大陆碰撞，不但令斗罗大陆面积增大了超过一倍，同时也带去了许多变数。
Especially four thousand years ago that the crustal movements of continental collision event, not only make the Douro mainland area increased more than one times, but also brought many variables.
然而，由于地壳的变动，那些包含着古代动植物尸体的沉积物重新回到了地球表面，在那里他们分解，并又一次的从大气中吸取氧气。
As the crust shifts, however, it can bring sediments containing ancient corpses back to the surface, where they decompose, removing oxygen from the atmosphere once more.
作者称这种地质变动现象为地质冰川运动，地质冰川运动普遍存在于上层地壳的运动之中。
The author of this paper classifies such phenomena of geologic changes as "geologic glacier movement" which, according to the author, extensively exists in the movement: of the upper crust.
是麻粒岩相变质作用发生于地壳大幅度增厚的环境，强烈的构造变动和区域性高热流共同作用的结果。
The above shows that granulite facies metamorphism occurred in the crust of (increasing) thickness and caused by strong tectonic disturbance and regional high heat flow.
是麻粒岩相变质作用发生于地壳大幅度增厚的环境，强烈的构造变动和区域性高热流共同作用的结果。
The above shows that granulite facies metamorphism occurred in the crust of (increasing) thickness and caused by strong tectonic disturbance and regional high heat flow.
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