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吉拉铜金矿位于冈底斯成矿带中段南缘,谢通门铜金富铁矿集区,与著名的雄村特大型铜金矿毗邻,成矿条件优越,化探异常显示Cu、Au、Pb、Zn、Ag元素标准差、变化系数大,富集能力强,元素套叠好,异常浓集中心突出,浓集中心与矿化(体)相对应,属典型的致矿异常,矿(化)体分布与大理岩和闪长岩接触带上。建议应以冈底斯成矿带铜多金属矿成矿找矿模式及雄村矿床的发现经验来指导找矿,继续加强勘查和研究工作,将有望实现斑岩型、矽卡岩型铜多金属矿,韧性剪切带型、蚀变岩性金铜矿的重大找矿突破。
The Gela copper-gold deposit is located in the southern margin of the middle section of the Gangdese metallogenic belt and is adjacent to the Tongtongmen copper-gold-rich iron ore concentration area adjacent to the famous Xiongcun extra-large copper-gold deposit. Its metallogenic conditions are superior and its geochemical anomalies show Cu, Au , Pb, Zn, Ag standard deviation, large coefficient of variation, enrichment ability, element nested well, abnormal concentration center prominent concentration center and mineralization (body) corresponding to a typical mineralization anomaly, ore (Chemical) body distribution and marble and diorite contact zone. It is suggested that prospecting should be guided by copper-polymetallic mineralization prospecting model in the Gangdese metallogenic belt and the discovery of the Xiongcun deposit. Continuing to strengthen the exploration and research work, it is expected that the porphyry-type and skarn- Metal ore, ductile shear zone type, alteration lithology gold and copper major breakthrough in prospecting.