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铀矿床的形成是在同生作用、成岩作用和后生作用参予下产生的。不同的研究者为适应具体的矿床给这些作用以不同的评价。在个别沉积矿床中,铀高度的富集,通常是与这些作用中之某一种有关,因而在普查类似的新矿床时,必须了解所有作用,其中包括金属原始同生堆积的作用,那怕这种作用是极微小的。在论文中作者没有提到铀-磷矿床及含铀砾岩矿床,因为这些矿床,作者看作为热液的或沉积变质的矿床。
The formation of uranium deposits is produced under syngenetic, diagenetic and epigenetic effects. Different researchers have different assessments of these effects in order to adapt to specific deposits. The enrichment of uranium heights in individual sedimentary deposits is usually related to any one of these effects and therefore all functions must be understood in census of similar new deposits, including the role of primitive symbiosis of metals, even though This effect is minimal. The authors did not mention uranium-phosphate deposits and uranium-bearing conglomerate deposits in the paper because these deposits were considered by the authors as hydrothermal or sedimentary metamorphic deposits.