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卡特巴阿苏金矿床位于新疆西天山中段,属那拉提-红柳河铜、镍、金、铁、铂族、白云母玉石成矿带,矿区内受那拉提北缘断裂(F2)的影响,发育次一级北东、北东东向断裂,使得含矿热液得以沿F5、F6之间破碎带上侵并赋存于其内的节理系统中,形成了面积较大的矿化带,在节理密集区域形成了一系列的矿体。故卡特巴阿苏金矿床具明显的断裂控矿、节理赋矿特征。
The Khatba Aso gold deposit is located in the middle of the western Tianshan Mountains in Xinjiang. It belongs to the Nalati-Hongliuhe copper-, nickel-, gold-, iron-, platinum- and muscovite jade metallogenic belt. It is fractured by the northern margin of the Nalati (F2) Influence and develop secondary and northeastern east-northerly faults, so that the ore-bearing hydrothermal fluids can invade and accumulate in the joint system along the fractured zone between F5 and F6, resulting in the formation of a large area of mineralization Belt, forming a series of ore bodies in densely knotted area. Therefore, the Carterba Aso gold deposit is obviously controlled by faults and controlled by ore-dressing.