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从前寒武纪至现代的岩石圈的发育中,岩石的塑性变形和构造流动具有突出重要的意义。构成岩石圈的巨大地质体的成分与性质是不同的,并按不同方式变形:巨大变形和空间变位、流散、断裂、相互滑移、积极参与十分复杂的岩石圈运动或者更恰当的说是岩石圈流动。岩石圈的构造圈层在很大程度上就是这种流动的结果。复杂的应力场、岩浆的形成、岩石的变质作用促进了构造流动并使构造流动复杂化。构造流控制矿床的分布和地震活动带的分布。因此,构造流的研究不仅在理论上尤其在实际上十分重要。
During the development of the lithosphere from the Precambrian to the modern, the plastic deformation and tectonic flow of the rock are of great significance. The composition and nature of the huge geologic bodies that make up the lithosphere are different and deform in different ways: huge deformations and spatial displacements, divergences, faults, and mutual slip, actively participating in very complex lithospheric movements or, more properly, The lithosphere is flowing. The formation of the lithosphere is largely the result of this flow. Complex stress fields, magma formation and metamorphism of rocks promote tectonic flow and complicate tectonic flow. Distribution of tectonic flow control deposits and distribution of seismic zones. Therefore, the study of tectonic flow is not only theoretically important but actually very important.