摘要
新疆卡特巴阿苏金铜矿床属于特大型金铜矿床。由于近些年才新开发出来,因此关于其矿床矿石特征与矿床成因的系统研究资料相对较少,故其研究具有一定意义。卡特巴阿苏金铜矿床位于我国新疆西天山那拉提结构带的北缘,受地层变化、地质结构以及岩浆热液等因素的影响而形成。矿床中的矿物质来自地层,含矿热液运移通道及容矿具体空间则来自地质结构。矿床形成的热动力来自岩浆热液。本文将围绕“新疆卡特巴阿苏金铜矿床矿石特征与矿床成因分析”这一话题进行研究和探讨。
The Katabela-Arsuk gold-copper deposit in Xinjiang,China is a giant gold-copper deposit.Due to its recent development,there is relatively little systematic research on the deposit's ore characteristics and genesis,making further study significant.The deposit is located in the northern part of the Narat-Tuokesu structural belt,western Tianshan Mountains,Xinjiang.The formation of the deposit was influenced by factors such as stratigraphic changes,geological structures,and magmatic hydrothermal activities.The deposit's mineral elements originate from the strata,with channels for ore-bearing hydrothermal fluids and specific ore-hosting spaces provided by geological structures.The thermal dynamics that drove the formation of the deposit are from magmatic hydrothermal activities.
作者
李锴强
LI Kai-qiang(The First Regional Geological Survey Brigade of Xinjiang Geological and Mineral Exploration and Development Bureau,Urumqi 830000,China)
出处
《世界有色金属》
2023年第21期70-72,共3页
World Nonferrous Metals
关键词
新疆
卡特巴阿苏金铜矿床矿石
特征
矿床成因
Xinjiang
Katabasu gold copper deposit ore
features
Genesis of ore deposit
