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大陆构造以受中地壳塑性层控制的盆－山系和冲叠造山带厚皮构造为主要构造类型，而与中生代以来才出现的受软流层控制的大洋岩石圈板块构造截然不同。由上地壳正断层上盘断陷盆地和下盘断隆山所组成的盆－山系，与地球自转速度逐渐变慢派生不同性质水平力和重力的共同作用有关。当地球自转速度突然变化时，将派生强烈的侧压力，使升降幅度较大、具有侧向应变空间的断陷盆地与断隆山之间的上地壳发生冲叠运动，盆－山系由此演变成冲叠造山带。后者对前者存在着严格的继承关系，服从于“升降－冲叠律”。中生代以来的盆－山系和冲叠造山带有的是板块活动产物
The continental structure is dominated by the basin-mountain system and the thick-skinned tectonic belt controlled by the plastic layer in the crust, but distinctly different from the oceanic lithospheric blocks controlled by the asthenosphere since the Mesozoic. The basin-mountain system, which consists of the upper crust faulted plate upper fault faulted basin and the lower crust fault mountain, is related to the combined effect of different horizontal forces and gravity derived from the gradual slowdown of the Earth’s rotation speed. When the Earth’s rotation speed suddenly changes, it will derive strong lateral pressure so that the amplitude of the lift will increase greatly. The upper crust between the fault basin with the lateral strain space and the fault mountain will have a superposition movement, and the basin-mountain system will evolve accordingly Into the orogenic belt. The latter has a strict inheritance relationship with the former and is subject to the “rise-fall-rush law.” Since the Mesozoic basin - mountain and overlying orogenic belt is the plate activities