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凡口铅锌矿床是发育于上古生界碳酸盐岩建造中的海底热泉喷溢矿床。在研究矿床地质的基础上 ,使用矿物包裹体测温方法 ,研究矿体温度场的分布 ,配合矿化元素的分布状态和矿石组构分带特征 ,推断成矿流体的喷口位置和运移方向
The Fankou lead-zinc deposit is a submarine hot spring spout deposit developed in the Upper Paleozoic carbonate rock formation. Based on the study of the geology of the deposit, the temperature distribution of the ore body is studied by using the method of temperature measurement of mineral inclusions. The distribution of mineralization elements and the zonation of the ore composition are deduced, and the position and direction of the nozzle of the ore-forming fluid are deduced