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关于对地球历史早期构造体制的认识,目前还在探索之中,但是,有一点大家的观点基本是一致的,那就是在太古宙时的“板块”(或称陆核)规模小。元古宙伊始,类似现代的板块构造机制制约地壳演化已越来越得到较多人的认同。不同的构造环境形成不同的构造岩石组合。对早前古生界构造环境的鉴别,人们往往多以构造岩石组合及其地球化学的环境属性作为标准。不论地热的来源如何,也不论它在总体规模上是如何散失的,它同构造应力共同作用下所造就的造山运动,形成宏伟的山链,则是呈现在眼前的地质事实。
The understanding about the early tectonic system of Earth’s history is still being explored. However, one point is basically the same. That is, the size of the “plate” (or ternary nucleus) in the Archean universe is small. At the beginning of the Proterozoic, similar to the modern plate tectonic mechanism restricting the evolution of the crust has been more and more people agree. Different tectonic settings form different tectonic rock assemblages. For the identification of the tectonic setting of the Paleozoic earlier, people tend to use the rock assemblage and its geochemical environmental attributes as the standard. Regardless of the source of geothermal energy and how it dissipates in the overall scale, the orogeny created by its joint action with tectonic stress and the formation of a magnificent mountain chain are the geological facts before us.