吉尔吉斯斯坦柯克苏矿田铜金矿地质特征及成因分析

摘要

吉尔吉斯斯坦柯克苏矿田内晚古生代碳酸盐岩地层发育,石炭一二叠纪岩浆活动强烈,以发育矽卡岩型铜金矿为主,次为构造蚀变岩型及热液型.矿体呈脉状、透镜状、似层状等,产于岩体及地层接触带上,受岩体、岩脉、地层及裂隙带共同控制.通过对左岸等5处矿床地质特征、成因类型、成矿规律的总结分析,认为在矿床深部具较好的找矿潜力.%Both lower Paleozoic carbonate strata and strong activity of the Carboniferous-Permian magma are favorable conditions for the Kirk Sue Ore Fields in Kyrgyzstan.This area mainly develop skarn deposit,with lesser tectonic altered rock type and epithermal deposit.Ore bodies are vein,lenticular,like a layer,etc.,which are found in rock mass and stratigraphic contact,strongly controlled by rock mass,dike,formation and fracture zones.Based on the analysis and summarize the geological characteristics,genetic type and regularity of the left bank,etc.Five deposits,believe in the deep deposit has good and prospecting potential.