与钠交代作用有关的铀矿床形成于花岗岩类和片麻岩构成的结晶地质内沿区域断裂构造带发育的钠长岩中。在前寒武系近地表的岩石中,钠交代和铀矿化都取决于超变质期后溶液的进入情况(此溶液含有碱性元素和铀)。多次发生的断裂构造复活导致钠长岩的形成,其中部分含有铀。 Uranium deposits related to the sodium metasomatism were formed in the albite developed in the fault zone within the crystalline geology of granitoids and gneisses. In Precambrian near-surface rocks, both sodium metasomatism and uranium mineralization depend on the entry of the solution after the ultra-metamorphic period (this solution contains alkaline elements and uranium). Repeated rupture of structures led to the formation of albite, some of which contain uranium.