Recently, a number of research findings have come to light about the age of plate tectonics, and energies are needed to operate it. The aim of present study is to investigate whether the energy of plate tectonics process was different during the Phanerozoic (Pz) and in earlier eons, and if there is such a discrepancy, whether it can be justified by changes in the processes that able to move the plates. The study will track temporal changes in important components of plate tectonics such as length of mid‐ocean ridges, subduction zones and relative oceanic crust coverage during Phanerozoic. Next, it will be examined how the knowledge gained in this way can be reconciled with the results of studies of previous eons. It was found that the temporal variation in kinetic energy of axial rotation due to changes in length of day (LOD) can be assumed as a determining energy which acts on the tectonic plates as in the Phanerozoic as earlier in Archean (Arch) and Proterozoic (Ptz).

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关于板块构造的能量和年龄

近来，有关板块构造时代的许多研究发现被揭露，并且需要能量来对其进行操作。本研究的目的是调查在古生代（Pz）和较早的年代板块构造过程的能量是否不同，如果存在这种差异，是否可以通过能够移动的过程的变化来证明其合理性。盘子。这项研究将追踪板块构造重要成分的时间变化，例如中生代期间中洋海脊的长度，俯冲带和相对的地壳覆盖率。接下来，将研究如何将以这种方式获得的知识与以前的世代研究结果相一致。