对铀矿床的形成,随着地质科学的发展,地质、水文地质,地球化学等资料丰富积累,从单一说逐渐形成多铀源、多阶段和多成因的观点,其中对地下热水后期改造已为铀矿地质工作者所注意。而这种古地下热水的后期成矿怍用,严格的受着古水文地质环境和古地下水的活动控制。这里所谓的古地下水,系指在第四纪以前来源于古大气降水的古常温地下水和 The uranium deposit formation, with the development of geological science, geology, hydrogeology, geochemistry and other information is rich in accumulation, from a single said that the formation of multi-uranium source, multi-stage and multi-genesis point of view, of which the late underground water has been transformed Note for uranium geology workers. The late underground mineralization of ancient underground water use, strictly controlled by the ancient hydrogeological environment and paleo-groundwater activities. The ancient groundwater, here refers to the paleo-temperature groundwater from the paleo-atmospheric precipitation before Quaternary and