环巴尔喀什-西准噶尔成矿省古生代地质演化的多阶段性,导致成矿物质强烈活化并多次迁移,形成了多个世界级的金属矿床。西准噶尔地区位于该成矿省的东段,其西部沿安齐断裂带发育一系列以哈图金矿、齐Ⅲ金矿为代表的金矿床和矿点,是区内规模最大的金矿聚集区,称为哈图成矿带(图1)。哈图和齐Ⅲ金矿位于安齐断裂上盘,NW、NE和EW向次级断裂是主要的容 The multi-stage geological evolution of the Paleozoic in the Balkhash-West Junggar metallogenic province led to the strong activation and multiple migration of ore-forming materials and the formation of several world-class metallogenic deposits. The west Junggar region is located in the east part of the metallogenic province, and a series of gold deposits and ore deposits represented by the Hatu gold and Qi Ⅲ gold deposits are developed along the Anqi fault in the west, which is the largest gold deposit in the area Area, known as the Hatha metallogenic belt (Figure 1). The Hetu and Qi Ⅲ gold mines are located on the upper Anzai fault and the secondary faults NW, NE and EW are the major ones