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松湖铁矿床和智博铁矿床位于阿吾拉勒石炭纪裂谷带东段。松湖铁矿先火山作用形成沉积型铁矿,后含矿热液加富矿床;智博铁矿是以岩浆作用为主热液作用为辅的复合型矿床。对阿吾拉勒成矿带上的松湖铁矿与智博铁矿从容矿地层、控矿构造、岩浆岩以及围岩蚀变特征方面加以总结对比,发现它们之间存在的异同之处,为阿吾拉勒地区铁矿或者其它成矿带找矿和预测提供理论指导。
The Songhu and Zhibo iron ore deposits are located in the eastern section of the Carboniferous rift zone in Awulal. Songhu Iron Mine volcano formed the first deposit of iron ore type, after the ore-bearing hydrothermal enrichment deposits; Ziboshi iron ore is the magmatic hydrothermal interaction-based composite deposit. Summarizing and contrasting the loose ore strata, ore-controlling structures, magmatic rocks and the alteration characteristics of surrounding rock in Songhu Lake Iron Mine and Zhibo Iron Mine in Uwulale metallogenic belt, we find that there are similarities and differences between them, The Lale area iron ore or other metallogenic belt prospecting and prediction provide theoretical guidance.