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1区域地质背景九顶山斑岩型铜钼金多金属矿床大地构造位置处于扬子板块西缘与金沙江-哀牢山深大断裂构造带东侧交会部位。而金沙江-哀牢山成矿带是西南三江地区重要的多金属成矿带之一,也是世界上著名的构造岩浆带之一,构造运动频繁,岩浆活动强烈,成矿作用特殊,形成了丰富多样的铜、钼、金多金属矿产资源。矿区内出露古
1. Regional Geological Background The geotectonic location of the Jinding Mountain porphyry copper-molybdenum gold polymetallic deposit is located at the intersection of the western margin of the Yangtze Plate and east of the Jinshajiang-Ailao Deep-seated tectonic belt. The Jinshajiang-Ailaoshan metallogenic belt is one of the important polymetallic metallogenic belts in the Sanjiang area of southwestern China. It is also one of the world famous structural magmatic belts with frequent tectonic movements, strong magmatic activity and special metallogenesis. Rich and varied copper, molybdenum, gold and polymetallic mineral resources. Ancient exposed in the mining area