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含铀混合岩大部分位于古陆隆起带边部、ＮＷ向花岗岩外接触带。深大断裂系统在成矿成岩中占有相当重要的地位。燕山期构造和岩浆活化，对原有的构造和矿化进行了强烈改造。在混合岩中发现了两种主要成矿类型，即铀一赤铁矿型和铀一碳酸盐型。
Most of the uranium-bearing mixed rocks are located at the edge of the ancient uplift belt and the outer contact belt of NW granite. The deep fault system occupies a very important position in mineralization and diagenesis. Yanshanian tectonism and magmatic activation, the original structure and mineralization have been strongly rebuilt. Two major metallogenic types have been identified in the mixed rocks, uraninite-hematite and uranium-carbonate.