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盆地的形成主要受地球演化的动力学机制的控制。由于地幔的抬升和调整是盆地形成的主要原因，地幔梯度带的倾向变化，决定了一些盆地的形态特点，即：引起盖层构造变化的原因，归结为深部构造的不同。在此基础上，将东北地区中新生代盆地划分为两类：第一类为由于地幔抬升机制控制的盆地；第二类为分布于古陆边部受地幔调整机制控制的盆地。除此之外，还有一类盆地，即受地体构造控制的盆地。并对其盖层构造的特点进行了讨论。
The formation of the basin is mainly controlled by the dynamical mechanism of the evolution of the earth. Since the uplift and adjustment of the mantle is the main reason for basin formation, the tendency of the gradient of the mantle gradient determines the morphological characteristics of some basins: the reason for the structural changes in the caprocks is attributed to the differences in deep structures. On this basis, the Mesozoic-Cenozoic basins in Northeast China are divided into two types: the first one is the basin controlled by the mantle uplift mechanism; the second one is the basin controlled by the mantle adjustment mechanism located on the edge of the ancient land. In addition, there is a type of basin, a basin controlled by the structure of the earth’s structure. The characteristics of its cover structure are also discussed.