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目前,在判明不同类型铀矿床的形成条件及分布规律方面取得了较大进步。在很大程度上是由于在矿床研究中采用了综合性的地质研究工作,从而考虑到不同的自然条件,其中包括各类成因的地下水在铀矿形成中的作用。
At present, great progress has been made in identifying the formation conditions and distribution rules of different types of uranium deposits. This is due in large part to the use of comprehensive geological studies in deposit studies that take into account different natural conditions, including the role of groundwater of all kinds of origin in uranium formation.