由于地球构造运动的复杂性以及一些著名的学者对构造运动学的概念有着各种不同的理解,构造运动的起源及其类型划分问题,迄今仍然处于讨论阶段,自地球作为一种地质体形成时起直到现在,在其核中一直保持着平衡状态,即密度、温度及物质成分在水平和垂直方向的不均匀性的均衡。这一点由于地球内部物质的垂直的和水平的迁移以及温度差的消失而得到实现。现时,这种机制显然包括着由地表至地心的全部深度。此外,地球体还周期性的变形,后者用一些地质现象(海侵、海退等)反映出来。在大多数场合下,构造运动不是根据其最初的发生原因分类,而是相反,根据其结果——由其形成的一些最主要的构造形态分类的。这是可以理解的,即我们被迫根据其结果即变形、相的分析及厚度、海岸线的迁移、物理地质过程的强度等等,并根据一些仪器测定指标 Due to the complexity of Earth’s tectonic movement and the famous scholars’ different understanding of the concept of tectonic kinematics, the origin of tectonic movement and the classification of its types are still in the discussion stage so far. Since the Earth was formed as a geological body Up till now, it has maintained a balance in its nucleus, that is, a balance of density, temperature, and inhomogeneity of material components in horizontal and vertical directions. This is achieved by the vertical and horizontal migration of matter inside the Earth and the disappearance of temperature differences. At present, this mechanism obviously includes the full depth from the surface to the earth’s core. In addition, the Earth also cyclically deformed, the latter with some geological phenomena (transgression, regression, etc.) reflected. In most cases, tectonic movements are not classified according to their original causes, but rather, on the basis of their result - classified by some of the most dominant tectonic forms they form. This is understandable in the sense that we are forced to rely on the results of deformation, phase analysis and thickness, coastline migration, the strength of the physical geologic processes, etc., and based on some instrumental measures