地幔圈

地幔圈形状周期性变化使地壳产生势能（位能）力导致地壳运动。

That the cyclical change of the shape of the mantle produces potential energy force in earth 's crust results in crustal movement .

岩石圈型块体在岩石圈尺度上是力学耦合的，以上地幔软流圈的顶面为其底部边界。

The latter is mechanically coupled in lithosphere scale , and consequently it lies on asthenosphere and the top of asthenosphere is regarded as its bottom .

自侏罗纪以来，该区地幔软流圈上涌，地壳拉张，控制中、新生代断陷盆地的形成与火山活动。

The upwelling of asthenosphere and extension of overlying lithosphere in Jurassic controlled the fault basins and volcanic actions in this area , which had high extension degree in Jurassic .

成盆动力学系统是一个包括沉积盆地及其下的地幔、软流圈、岩石圈和莫霍面等不同地质单元的宏观变化和相互制约的过程。

Sedimentary basin forming dynamics system is the macroevolution and correlation of the sedimentary basin , the mantle , the asthenosphere , the lithosphere , and Moho discontinuity .