铀矿床同其他金属矿床一样,大多数类型在世界许多地方都是相似的。这些矿床都是由少数已被认识的地质过程、物理和化学控制因素形成的。这些控制因素从大到小,可归纳为:从板块构造、全球的、各大洲的或区域性的造山运动或金属成矿分带到区域或局部的岩浆活动、侵蚀-沉积作用、溶解-沉淀作用等。还有更细小的构造控制作用,其活动范围仅为几厘米到几米。在许多矿产远景不明的地区,同样发现了 Uranium Deposits Like other metal deposits, most types are similar in many parts of the world. These deposits are formed by a few well-known geological processes, physical and chemical control factors. These control factors from largest to smallest can be summarized as tectonic movements from plate tectonics, global or continent or regional orogenies or metallogenic mineralization to regional or local magmatic activities, erosion-sedimentation, dissolution-sedimentation Role and so on. There are finer structure control, the scope of its activity is only a few centimeters to a few meters. The same is true in many areas where the mineral is far from clear