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铀矿化产于超覆硅质岩的红色砾岩接触带的下盘。容矿构造类型包括:被顺层断裂和切割断裂复杂化了的褶曲翼部和转折端; 在断裂交错中岩石裂隙度提高的地段; 伴随切割断裂的裂隙和破碎带。矿化的产出取决于固岩脆性变形的能力。矿期蚀变为赤铁矿化和绿泥石化。成矿热液中,当铀酰络合物分解和六价铀被两价铁还原时,铀从热液中沉淀出来。
Uranium mineralization occurs in the lower disk of the red conglomerate contact zone of supergiated cherts. The types of ore-hosting structures include: folded wing sections and turning ends that are complicated by bedding faults and cutting faults; areas where fractures of rocks are enhanced during fracture interlacing; fractures and fractures that accompany cutting faults. The output of mineralization depends on the ability of the rock to become brittle. Ore alteration to hematite and chloritization. In the hydrothermal fluids, uranium precipitates from hydrothermal fluids when uranyl complex is decomposed and hexavalent uranium is reduced by divalent iron.