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钠-铀建造矿床赋存于钠长岩中。它与复杂结构的区域断裂构造带中的花岗岩类和片麻岩的碱交代作用有关。碱交代作用见于各类碱性交代岩的形成过程中。根据交代作用的强弱可将这些岩石分为:钠长岩、似正长岩的去硅岩石和弱碱性岩。铀矿化主要产于钠长岩中,即花岗岩类和片麻岩经彻底交代的产物中。而且它基本上是成分复杂的铀钛酸盐。确定钛在铀矿形成过程中的性状,有助于这类建造的矿床形成条件的研究。建筑在高电势、电子亲合势、负电性及其它资料基础上的,关于化学元素的共生的理论概念,可使人们把
Sodium-uranium deposits occur in albite. It is related to the alkali metasomatism of granitoids and gneisses from the regional structural zone of complex structure. Alkali metamorphism is found in the formation of various alkaline metamorphic rocks. These rocks can be divided into albite, deformable rocks and weakly alkaline rocks that are similar to syenite based on the intensity of metasomatism. Uranium mineralization is mainly produced in albite, the product of granite and gneiss that has been thoroughly accounted for. And it’s basically a complex uranium titanate. Determine the characteristics of titanium in the formation of uranium deposits, contribute to the formation of such deposits to study the conditions. Building on the theory of high potential, electron affinity, negative charge and other data, the symbiosis of chemical elements allows one to