浅论新疆哈密市银帮山铜多金属矿地质特征及找矿标志

Brief Discussion on Geological Characteristics and Prospecting Sign of Yinbangshan Copper Polymetallic Deposit in Hami City, Xinjiang

新疆哈密市银帮山铜多金属矿区,地处雅满苏石炭系岛弧带东部,以及苦水断裂与沙泉子深大断裂的中间地带。矿区南段是中部天山成矿区,其北部是黄山成矿区。本文结合对矿区成矿地质条件的分析,从矿床地质特性着手,研究了成矿的条件以及矿化的蚀变性能,给出了找矿标志,从而为后续在该区域的地质勘探工作提供一定的技术支持。

The Yinbangshan copper polymetallic ore district in Hami City, Xinjiang, is located in the eastern part of the Arctic Su Carboniferous Island Arc Belt and the middle zone between the Kushui Fault and the Shaquanzi Deep Fault. The southern section of the mining area is the central Tianshan metallogenic area, and the northern part is the Huangshan metallogenic area. Based on the analysis of the ore-forming geological conditions of the mining area, the geological characteristics of the deposit are studied. The conditions of mineralization and the alteration performance of mineralization are studied. The prospecting mark is given, which provides a certain post-geological exploration work in the area. Technical support.