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捷列托夫斯卡河铀矿床产于第三纪斜辉熔岩中,这种岩石是在捷列托沃-克拉托沃成矿区火山活动后期形成的。铀很大可能是来源于斜辉熔岩固结后活化的深部岩浆源。因此,铀矿床与斜辉熔岩的关系是共生的,而不是直接成因的。矿化为断层构造所控制。矿体主要是脉型的,产于剪切带内。矿床在热液活动的浅成相及矿化过程的最后某一阶段内形成。铀矿化沉积于硫化物矿化主要相之后,由手硫化物的矿化作用,产生了捷列托沃-克拉托沃地区重要的铅锌矿床。沉积次序明显,首先是铜、其次是铅-锌,最后为铀矿化。这种矿物共生组合形成已反映于其明显的分带性上,它表明矿化溶液的这种分异作用引起热液活动后期铀含量的增加,并形成捷列托夫斯卡河铀矿床。
The Teretovskaya uranium deposit was produced in Tertiary glaucoma formed later in the volcanic activity of the Teretovo-Kratov mineralization. Much of the uranium is likely to have originated from deep magmatic sources activated by the consolidation of obliquely lava. Therefore, the relationship between uranium deposits and beryl lavas is symbiotic, not direct. Mineralization is controlled by fault structure. The ore body is mainly vein-shaped, produced in the shear zone. The deposit formed during the last phase of the shallow facies and mineralization of hydrothermal activities. After uranium mineralization is deposited on the major facies of sulphide mineralization, the mineralization of the hand sulphide produces an important lead-zinc deposit in the Terretovo-Kratovo region. The order of deposition is obvious, first copper, followed by lead-zinc, and finally uranium mineralization. The formation of this symbiotic assemblage has been reflected in its apparent zonation, which indicates that this differentiation of mineralization solutions led to an increase of uranium content during the late hydrothermal activity and the formation of the Teretovska uranium deposit.