经过陕西省地矿局第六地质队广大地质职工多年工作,现已查明一个特大型碳酸岩型铀铝矿床,并肯定了其工业价值。 该矿床位于华北地台南缘、汾渭裂谷南侧,太行新华夏隆起带与秦岭纬向构造带北亚带的交汇部位,与铁岔沟碳酸岩型铁矿,黄龙铺碳酸岩型钼、铅矿,驾鹿碳酸岩型稀土矿同处于一个碳酸岩带上。 After many years of working for the geological staff of the Sixth Geological Team of Shaanxi Provincial Bureau of Geology and Mineral Resources, an extra large carbonate-type uranium-aluminum deposit has been identified and its industrial value has been affirmed. The deposit is located in the southern margin of North China Platform, south of Fenwei Rift, the junction of the Taihang New Huaxia Uplift and the north subtropical zone of the Qinling zonal structural belt, with the Tiechagou carbonate rock type iron ore, Huanglongpu carbonate rock type molybdenum, Lead ore, deer carport-type rare earth ore with a carbonate zone.