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新疆且末县木孜塔格铁矿成矿单元划归为昆仑成矿省喀拉米兰铜钴锌金银成矿带之喀拉米兰(复合沟弧带)金铜银矿带,构造单元为阿尔金超深大断裂南部的塔里木陆块南缘活动带喀拉米兰晚古生代弧沟系[1],与其东侧的卡特里西铜锌矿属同一构造单元和成矿背景,赋矿地层为下石炭统托库孜达坂群,含矿岩性为基性凝灰岩。通过对木孜塔格铁矿床成因分析和总结找矿标志,对在该成矿带进一步开展找矿工作具有积极指导意义。
The Muzittag iron ore-forming unit in Qiemo County of Xinjiang is classified as the Kelalanlan (composite groove arc) gold-copper-silver ore belt of the Kelalanlan copper-cobalt-zinc gold-silver metallogenic belt in the Kunlun Mountains and the tectonic unit is Altyn- Late Cretaceous arc groove system [1] in the southern margin of the Tarim block in the southern part of the ultra-deep fault with the same tectonic unit and metallogenic background as the Catrellizite in the east of the area. The ore-bearing strata are Carboniferous Tong Tuo Kou Daban group, ore-bearing lithology is the basic tuff. Through the analysis of the genesis of the Muztagal iron deposit and the conclusion of ore prospecting marks, it is of guiding significance to further carry on the prospecting work in this metallogenic belt.