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铀矿床主要产于下石炭统石磴子组灰岩中,铀矿化主要受地层、岩相和后期构造控制,地下水和地下循环热水对成矿也起了重要的作用。该矿床为层控矿床,它是长时间、多阶段、复成因的,主要经历了沉积、成岩矿化、古地下水成矿、古地下热水迭加成矿、现代地下水的破坏与继积成矿五个阶段。
Uranium deposits are mainly produced in the Lower Carboniferous Shijiazui limestone. Uranium mineralization is mainly controlled by strata, lithofacies and post-tectonics. Groundwater and subsurface hot water also play an important role in metallogenesis. The deposit is a stratum-controlled ore deposit. It is a long time, multi-staged and complex formation. It mainly experienced sedimentation, diagenesis and mineralization, mineralization of paleo-groundwater, superimposition and mineralization of paleo-underground hot water, destruction of modern groundwater and subsequent accumulation Mine five stages.