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汗吉尕多金属成矿带位于新疆西天山 ,是一个以铅、锌、铜为主的多金属成矿带 ,该成矿带隶属于中亚成矿域巴尔喀什成矿带 ,其构造特点呈网格镶嵌断块结构 ,区内华力西期火山侵入活动发育 ,在哈萨克斯坦境内发现不少大型、超大型铜、铅锌矿床 ,如著名的科翁腊德、阿克斗卡、科克赛斑岩铜矿、捷克利铅锌矿等。经分析发现 ,汗吉尕多金属成矿带成矿地质背景、构造条件无疑是巴尔喀什成矿带延入我国的一部分 ,具备形成大型矿床的地质条件。
Khan-Ji-Ga polymetallic metallogenic belt is a polymetallic metallogenic belt dominated by lead, zinc and copper in the western Tianshan, Xinjiang. The metallogenic belt belonged to the Balkhash metallogenic belt in Central Asia, and its structural features Mesh mosaic block structure, the region during the Wahlixi volcano intrusion development, found in Kazakhstan in many large, super-large copper, lead-zinc deposits, such as the famous Keworde, Aktauka, Section Kesai porphyry copper, Czech Republic, lead-zinc and so on. After analysis, it is found that the metallogenic geological background and structural conditions of the Kijiji Ga polymetallic metallogenic belt are undoubtedly part of the Balkhash metallogenic belt extending into our country, with the geological conditions for forming a large deposit.