新疆地壳演化经历了长期复杂的历史过程,造山带在不同构造阶段、不同地球动力学环境下形成不同沉积建造及岩浆建造,与之对麻形成各种成矿类型.造山带经历了离散、汇聚、碰撞、陆内造山等阶段,每一阶段都有其特有的成矿地质背景.根据新疆具体情况,进行构造演化阶段的划分,建立构造演化序列.在综合研究基础上,划分不同大地构造环境下不同大地构造相类及构造相,并对其含矿特征进行了概述.
The crust evolution of xinjiang have experienced long-term and complex historical process, on the different tectonic stages and geodynamic environments, the orogenic belts is forming different sedimentary formation and magmatic formation, Corresponding to various features of metallogenic types.the belts have undergone different stages of splitting, amalgamation ,collision and intra-continent orogeny, every stage has its own metallogenic background.according to Xinjiang's special details,we divided the tectonic evolution stages,established the tectonic evolutionary series;on the basis of Comprehensive research,We divide tectonic faces catrgory and tectonic facies under the different geodynamic environment,Moreover, the ore-beating features of the belts are summarized.