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阿尔泰山南缘地区东部与西部地壳岩石构造变形特征与变质岩岩石组合显示该区地壳岩石变形可划分出两个不同的构造变形域 ,不同构造变形域内的构造形迹、构造样式、变质岩组成等方面存在明显差异。整个南缘地区的岩石变形变质呈现出东西分区、南北分带的总体格架 ,而形成这一构造格架的原因是两个不同构造变形域具有不同的变质基底及不同的岩石变形方式与变形机制
Deformational characteristics of the crustal rocks in the eastern and western parts of the southern margin of the Altay Mountains and their combination with metamorphic rocks show that crustal deformation in the crust can be divided into two different tectonic deformation zones, tectonic patterns, structural styles and metamorphic rock compositions in different tectonic deformation zones There are obvious differences. The deformation and deformation of the rock in the whole southern margin show the general framework of east-west division and north-south division. The reason for the formation of this tectonic framework is that two different deformation zones have different metamorphic basalts and different rock deformation modes and deformations mechanism