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西准噶尔地区位于中亚造山带西南缘,以大量中酸性侵入体广泛分布为特征,其中以达尔布特构造—岩浆带最为显著,其性质和期次对于认识该构造带的演化过程及其成矿效应具有十分重要的意义(韩宝福等,2006;申萍等,2008;李永军等,2012)。目前已发现包古图斑岩型铜矿床、哈图金矿床、苏云河石英脉—云英岩型钼矿床等,以及新近发现的吐克吐克、宏远铜、钼矿点等,是重要的成矿远景区,长期以来受到了地质找矿工作者的广泛关注,对其晚古生代构造—岩浆—成矿作用的研究一度成为地学研究的热点之一。本
The West Junggar region is located in the southwestern margin of the Central Asian orogenic belt and is characterized by the widespread distribution of a large number of intermediate-acidic intrusions. The Darbot tectonic-magmatic belt is most prominent. Its nature and period are of great significance in understanding the evolution of the structural belt and its evolution Mine effect is of great importance (Han Baofu et al., 2006; Shen Ping et al., 2008; Li Yongjun et al., 2012). It has been found that the Baotu Tu porphyry copper deposit, the Hatu gold deposit, the Suyunhe quartz vein-dolomitic molybdenum deposit, and the newly discovered Tuuktuk, Hongyuan copper and molybdenum ore deposits are important Has long been widely concerned by geological prospecting workers. The study of its Late Paleozoic tectono-magmatic-mineralization has been one of the hot topics in geosciences research for a time. this