论文部分内容阅读
矿体产于上三叠统图姆沟组与印支期复式中酸性斑(玢)岩体接触带矽卡岩化蚀变带中。岩浆岩、围岩碳酸盐岩地层、热液运移和矿质沉淀的构造空间控制了本矿床的产出。属较典型的矽卡岩型铜矿床。
The orebodies are produced in the skarn alteration zone in the contact zone between the Upper Triassic Tumbu Formation and Indosinian intermediate-acidic plagioclase rock. The production of magmatic rocks, surrounding rock carbonate formations, hydrothermal migration and mineral deposits control the output of this deposit. Is a more typical skarn copper deposit.