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373矿床是产于碳酸盐岩系中的一个大型铀矿床,除铀外,Mo巴构成矿床规模,Sb、Ni、V也可综合利用:并另发现了W异常,推测其深部可能形成矿化。 矿床产于地穹前缘古叠置型岩溶洼地中的地洼初动期岩溶沉积体中;矿体赋存于沉积体中下部。古叠置型岩溶洼地是地洼阶段多期岩溶作用形成,在遥感图象上呈环形影象——环洼。成矿物质来源于陆源吸取,在细菌作用下富集成矿。
373 deposit is a large-scale uranium deposit that is produced in carbonate rocks. In addition to uranium, Mo-Ba constitutes the size of the ore deposit. Sb, Ni, V can also be used in combination: another W anomaly is found, The The ore deposit is produced in the dipping primordial karst sediments in the ancient overlying karst depressions on the front of the dome of the vault. Ore bodies occur in the lower part of the sedimentary bodies. The ancient superimposed karst depression was formed by multi-stage karstification in the Diwa stage, showing a ring-shaped image on the remote sensing image - the ring depression. Metallogenic materials derived from terrestrial sources, enriched in the role of bacteria in mineralization.