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库鲁克塔格是新疆前寒武纪出露较全的地区,然而该区区域成矿规律研究程度非常低.通过对研究区已有资料进行总结分析,系统阐述研究区矿床类型,并对其成矿系列进行划分.研究区从太古代到早古生代形成了7个主要的岩浆构造演化阶段:古太古代陆核形成阶段(3.3~3.0Ga)、新太古代-古元古代陆壳增生改造阶段(2.6~2.3Ga)、古元古代中晚期陆壳改造阶段(2.1~1.8Ga)、中元古代晚期-新元古代早期造山运动阶段(1.1~0.86Ga)、新元古代中期后碰撞伸展阶段(830~800Ma)、新元古代中晚期陆内裂解阶段(770~600Ma)和早古生代造陆运动阶段.成矿作用主要发生在古元古代、新元古代及早古生代.依据各构造演化阶段、含矿建造特征及矿床成因特征,将库鲁克塔格成矿作用类型总结为以下6个主要成矿系列,即形成于古元古代陆壳增生改造环境下的Fe-P-Cu-Au系列、新元古代俯冲碰撞环境下的Cu-Au系列、新元古代后碰撞环境下的Cu-Mo-Au-Fe-P-REE系列、新元古代裂解环境下的Cu-Ni系列、早古生代沉积盆地中Ag-V-Mo-Au-U-P系列和早古生代俯冲岛弧环境下的Cu-Au系列.
Kuluke Tagu is a region exposed by the Precambrian in Xinjiang, however, the degree of metallogenic regularity in this area is very low.Through the summarization and analysis of the existing data in the study area, the type of deposit in the study area is expounded systematically, And its metallogenic series are divided.The study area has formed seven major stages of magmatic tectonic evolution from the Archean to Early Paleozoic: the Paleolithic continental nucleus (3.3 ~ 3.0Ga), the Neoarchean-Paleoproterozoic continental crust During the reconstruction stage (2.6-2.3 Ga), the late Paleoproterozoic continental crustal reformation (2.1-1.8Ga), the late Proterozoic-Early Neoproterozoic orogeny (1.1-0.86Ga), the Neoproterozoic metaphase post-collision (830 ~ 800 Ma), the Neo-Neoproterozoic intracontinental pyrolysis stage (770-600 Ma) and the Early Paleozoic land-forming movement.The mineralization took place mainly in the Paleoproterozoic, Neoproterozoic and Early Paleozoic.According to the tectonic evolution Stage, ore-bearing characteristics and ore-forming characteristics, the types of Kuruktag mineralization are summarized into the following six major metallogenic series: the Fe-P-Cu- Au series, the Neoproterozoic subduction collision environment Cu-Au series, the Cu-Mo-Au-Fe-P-REE series in the Neoproterozoic post-collision environment, the Cu-Ni series in the Neoproterozoic pyrolysis environment, the Ag-V-Mo-Au -UP series and the Cu-Au series of the Paleozoic subduction island arc environment.