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东天山秋黄韧性剪切带位于新疆东部两大板块碰撞接合地带，东西延长逾６００ｋｍ，由石炭系组成，规模巨大，分带明显，宏微观变形标志清晰，石英Ｃ轴组构呈点极密型，分为四期变形，序列演化明显，应变测量属平面单剪，剪切位移量达７５ｋｍ以上，存在脆韧性变形转换，变形时代为海西中晚期，强弱应变相间排列的标度不变性特征明显，变形机制属地壳中深层次塑性流变和韧性剪切，与板块间的俯冲碰撞构造演化密切相关。控制着金铜矿分布。
The East Tianshan Qiuhuang ductile shear zone is located in the collision zone of the two major plates in the eastern part of Xinjiang. The east-west extension of over 600km consists of the Carboniferous. It has a large scale with obvious zonation, clear macro-micro deformation marks, Type, which is divided into four stages of deformation, the sequence evolution is obvious, the strain measurement is a single shear plane, the shear displacement of more than 75km, brittle and ductile deformation of the existence of transition, the deformation of the middle and late Hercynian, the strength of the strain phase arrangement of the scale is not Deformation characteristics are obvious. The deformation mechanism belongs to deep crustal ductility and ductile shear, which is closely related to tectonic evolution of subduction collision between plates. Control the distribution of gold and copper.