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地壳均衡, 均衡平衡
the gravitational balance between Earth's rigid lithosphere and the underlying, semi-fluid asthenosphere, influencing variations in surface elevation
- The rebound of land following the melting of glaciers is a classic example of isostasy, where the crust adjusts to changes in load.
冰川融化后土地的反弹是地壳均衡的经典例子，地壳会根据负荷的变化进行调整。
- The formation of deep ocean basins, like the Pacific Ocean, is influenced by isostasy as dense oceanic crust sinks into the mantle.
像太平洋这样的深海盆地的形成受到地壳均衡的影响，因为密集的海洋地壳沉入地幔。
- The concept of isostasy helps explain the elevated elevations of continental shields, where thicker crust extends beneath the Earth's surface.
地壳均衡的概念有助于解释大陆地盾的高海拔，那里较厚的地壳延伸到地球表面以下。
- The concept of isostasy is crucial in understanding the dynamics of crustal movement and subsidence in areas with sedimentary basins.
地壳均衡的概念对于理解沉积盆地区域地壳运动和沉降的动力学至关重要。
- Isostasy is a fundamental principle in geophysics, guiding our understanding of the dynamic balance between Earth's rigid and fluid layers.
地壳均衡是地球物理学中的一个基本原则，指导我们理解地球刚性层和流体层之间的动态平衡。