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根据东天山及邻区地层、沉积建造、构造岩石组合、变形、变质、古生物分区、深部地壳结构、地球物理、地球化学特征，以康古尔塔格－黄山深断裂为界，划分了不同级别的构造单元和构造沉积相带。统计分析了２０２个金属矿床，重点研究了金、银、铜、镍、钼、铁等矿产空间分布与板块构造、碰撞带关系，划分出九个成矿带，三个成矿期，以海西中晚期最为显著。成矿与板缘构造活动带地质演化密切相关，与俯冲一碰撞带和韧性剪切带时空演化最为密切。构造分区控制的矿产成带性和构造演化形成的成矿集中期之间相互转化对该区金属矿产有重要控制作用。
According to the strata of East Tianshan and its adjacent areas, the sedimentary structures, tectonic assemblages of rocks, deformation, metamorphism, palaeontology, deep crustal structure, geophysics and geochemistry, and the Kanggutage-Huangshan deep fault as the boundary, Of tectonic units and structural sedimentary facies belt. Tens of metallogenic deposits are analyzed statistically. The relationship between the distribution of gold, silver, copper, nickel, molybdenum, iron and other minerals and the tectonic setting and collision zone are mainly studied. Nine metallogenic belts, three metallogenic stages, The most prominent in the middle and late. The mineralization is closely related to the geological evolution of the tectonic activity belt along the margin, and is most closely related to the temporal and spatial evolution of the subduction-dune collision zone and the ductile shear zone. The mutual conversion between the mineral belt-forming property controlled by tectonic zoning and the metallogenic concentration period formed by tectonic evolution plays an important role in controlling the metallogenic deposits in this area.