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本文综合了一些野外实际地质资料和11个矿区35个矿床的有关资料,认为成矿作用是一个复杂的地质过程。铀源层是成矿的物质基础,成矿岩体的自变质作用是成矿的充分条件,构造及风化剥蚀作用是成矿的必要条件。成矿岩体几乎无例外地都产于区域性的含铀层位分布区内,
This paper synthesizes some actual geological data in the field and 35 related deposits in 11 mining areas, and considers that the mineralization is a complicated geological process. The uranium source is the material basis of mineralization. The self-metamorphism of metallogenic rocks is a sufficient condition for metallogenesis. The tectonism and weathering and denudation are the necessary conditions for metallogenesis. Nearly without exception, the ore-bearing rock masses are all produced in the regional distribution area containing uranium,