【摘要】 红石铜矿地处东天山大南湖-头苏泉岛弧带北段的卡拉塔格地区。矿体产于奥陶系大柳沟组火山岩中,呈脉状产出,区内构造对矿体起着明显的控制作用。该区褶皱与断裂构造比较突出,侵入岩较发育,具有非常优越的成矿地质条件,找矿潜力巨大,因此成为研究的热点。该矿矿床成因为中低温火山热液型铜矿床。下文结合实践对该矿地质特征进行分析的基础上探讨其矿床成因,以供参考。更多还原

【Abstract】 The Hongshi copper deposit is located in the Karatag area of the northern part of the Dananhu-Tousuquan Island arc belt in the eastern Tianshan Mountains. The ore bodies occur in the volcanic rocks of the Ordovician Daliugou Formation and are vein-like. The structure in the area plays an obvious role in controlling the ore bodies. The folds and faults in this area are prominent, the intrusive rocks are well developed, and they have excellent metallogenic geological conditions.They have great potential for prospecting. Therefore, they have become a research hotspot. The genesis of the deposit is a medium-low temperature volcanic hydrothermal copper deposit. Based on the analysis of the geological characteristics of the deposit, the genesis of the deposit is discussed for reference.更多还原