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地下水在成矿过程中的特殊作用与携带一系列成矿物质的大量层状水、裂隙水和潜水的高容矿性和活动性有关。形成水成铀矿床的外生后成过程,也是地下水地质作用的结果。已有文献详细讨论过反映铀矿石后生成矿实质的放射性水文地球化学分带性。形成层状氧化带的含氧水中的铀,停留在氧化还原界面上,并形成铀的矿化带。矿化带向下顺着水流方向渐
The special role of groundwater in metallogenesis is related to the high volume mineral and activity of a large number of stratiform, fissured and subducted waters that carry a range of metallogenic materials. The formation of hydrothermal uranium deposits after the process, but also the result of groundwater geological effects. The literature has discussed in detail the true hydrogeochemical zonation of uranium ore after the formation of ore-forming radioactivity. The uranium in the oxygenated water that forms the layered oxidation zone stays at the redox interface and forms a mineralized zone of uranium. Mineralization belt down the direction of the water gradually