摘要
碳硅泥岩型铀矿化是红层（盆）外的一种重要矿化现象，二者不仅同源、同时和同区，而且有着因果联系。文中还探讨了碳硅泥岩型铀矿化出现的基本条件、成矿模式及找矿方向等问题。
The carbonate siliceous-pelitic rock uranium mineralization is an important mineralizationphenomenon outside the Red Bed. Both not only have the same source,same time and same area,butalso have the relationship of cause and effect.This paper also investigates the problems of basic condi-tions,mineral-forming models and prospecting direction appeared in the carbonate siliceous pelitic rockuranium mineralization.
出处
《华东地质学院学报》
1994年第1期68-75,共8页
Journal of East China Geological Institute
关键词
铀矿床
碳硅泥岩型
成矿作用
红层
Red beds
uranjum mineralization
carbonate siliceous-pelitic rock type
uranium oredeposits
mineralization models
