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通过对新疆阿尔泰南缘东段地区主要构造带变形岩石的X光岩组分析,认为该区岩石变形比较强烈,石英变形机制以中低温底面型或近底面型滑移为主,部分为中高温柱面Ⅰ型滑移系。属于中浅—中等层次(10～15km,T=300～450℃,p=0.25～0.40GPa)的韧脆性—韧性变形。达拉维孜-阿热勒托别剪切流变构造带和库尔提-玛因鄂博韧性剪压变形带变形的物理化学条件相似,结合区域地质分析,这2个带与萨尔布拉克-科克萨依脆性挤压劈理化带一起可能组成一个完整的板块(微陆块)聚合变形带。而锡泊渡(635水库)-富蕴变晶糜棱岩带岩石变形的条件明显不同,温度压力偏高,说明其具有不同的演化历史,可能为古生代期间被强烈改造的具有前震旦纪结晶基底的微大陆的残留。
Based on the analysis of the X-ray lithofacies of the deformed tectonic belts in the eastern margin of southern Altay, Xinjiang, it is considered that the deformation of the rocks is relatively strong. The deformation mechanism of the quartz is dominated by low-moderate or near-bottom-type skidding and partly by medium- and high-temperature Cylindrical type Ⅰ slip system. Which belongs to the ductile-ductile deformation of middle-shallow-middle-level (10 ~ 15km, T = 300 ~ 450 ℃, p = 0.25 ~ 0.40GPa). The Dalawiz-Athelet no-shear rheological structural zone is similar to the physical and chemical conditions of the deformation of the Kulti-Menebo ductile shear zone, combining with the regional geological analysis, - Coxa’s brittle extrusion of the cleavable belt together may form a complete plate (micro-block) polymerisation zone. The conditions of rock deformation in Xipudu (635 reservoir) -Fuyun metamorphic rock zone are obviously different, and the high temperature pressure indicates that they have different evolutionary history. They may have been characterized by pre-Sinian crystallization strongly modified during the Paleozoic The residual of the micro-continent of the basement.