摘要
Abstract
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.关键词
新疆/卡特巴阿苏金铜矿床矿石/特征/矿床成因Key words
Xinjiang/Katabasu gold copper deposit ore/features/Genesis of ore deposit分类
天文与地球科学
