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诸广—九在地区富铀矿床的典型沥青铀矿，明显地表现为低温浅成的晶胞参数、含氧系数等标型特征及矿石放射性同位素特征，表明富铀矿区的铀成矿作用是在原生热液成矿作用的基础上叠加有后生水成（淋积）作用。富铀矿区黑色岩系中过成熟及石墨化的有机（炭）质，为铀的水成（淋积）成矿提供了优越的环境。
The typical asphaltic uranium deposits of ZhuGuang-Jiuli ultra-rich uranium deposit are obviously characterized by low-temperature supergene unit cell parameters such as unit cell parameters, oxygen content and ore radioisotope characteristics, indicating that the uranium mineralization in the uranium-rich uranium deposits is On the basis of the protolith hydrothermal mineralization superimposed with epigenetic water into (Lin) role. The matured and graphitized organic (carbon) in the black rock series of the uranium-rich uranium deposits provide a superior environment for hydrothermal (mineralization) uranium mineralization.