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现在对于数量级达到几百米,大约1—10cm/千年的区域性海平面变化,Cloetingh等提出了一种新的构造机制。如果岩石圈内存在着几千巴数量级的水平应力,那么他们的模式就可解释上述的变化。应力场随着地质时代而变化。上述模式表现了应力场和由沉积载荷引起的岩石圈偏斜之间的相互作用(图1)。通过这种互相作用,在沉积盆地的边缘可以产生大於100米的显著的海平面变动。因此,Cloetingh等人指出,冰川变动不是产生显著的海
Now for a sea level change of magnitude of several hundred meters, about 1-10 cm / mil, Cloetingh et al. Propose a new structural mechanism. If there are horizontal stresses on the order of a few thousand bar in the lithosphere, their patterns explain the above changes. The stress field changes with the geologic age. The above model shows the interaction between stress field and lithospheric deflection caused by sedimentary load (Figure 1). By this interaction, significant sea-level variations greater than 100 meters can be produced at the edge of the sedimentary basin. Thus, Cloetingh et al. Point out that glacial change does not produce a significant sea