双龙铜矿地质特征及矿床成因浅析

Brief Analysis of Geological Characteristics and Genesis of Shuanglong Copper Deposit

双龙铜矿地处东天山觉罗塔格山系东部。矿体产于石炭系底坎尔组火山岩中,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。通过对矿床地质特征的分析,认为该矿床成因为中低温火山热液铜矿。

The Shuanglong copper deposit is located in the eastern part of the Jurotag arer in the eastern Tianshan Mountains.The ore bodies occur in the volcanic rocks of the Carboniferous Dikaer 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.Based on the analysis of the geological characteristics of the deposit.The genesis of the deposit is a medium-low temperature volcanic hydrothermal copper deposit.