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矿床地质概况该矿床是我国目前仅有的一个钨、铀伴生矿床。矿床位于某古隆起东南缘的一个向斜盆地中,矿区出露地层有元古界板溪群上亚群、震旦系、寒武系、奥陶系、石炭系,西侧为一复式花岗岩体。泥盆系是矿区的含矿地层,分下统、中统和上统。下统为底砾岩,中统应堂组为碎屑岩及东岗岭组白云岩及灰岩,上统榴江组为白云岩、粉砂质白云岩及泥灰岩等。矿区内的F_1和F_2断裂是控制铀、钨矿化的
Geological Overview of the deposit The deposit is the only one of our country tungsten, uranium associated deposits. The deposit is located in a syncline basin in the southeastern margin of a paleohigh. The outcrop formations in the mine area include the Upper Proterozoic Bangxi Group, Sinian, Cambrian, Ordovician and Carboniferous facies, and a compound granite to the west body. Devonian is the ore-bearing strata in the mining area, divided into lower, middle and upper strata. The lower member is the base conglomerate, the Zhongyou Yingtang Formation is clastic rock and the Donggangling Formation dolomite and limestone, the upper Lihe Formation is dolomite, silty dolomite and marl. F_1 and F_2 faults in the mining area are controlled by uranium and tungsten mineralization