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(1)经过“涅瓦国营地质企业”、全俄地质研究所和其他单位多年的铀矿预测-普查专门工作划分出了奥涅加-拉多日铀矿省。众多的铀矿点和一些小型铀矿床和大型综合铀-钒矿床大量放射性地球化学和放射性测量异常的发现,以及存在形成铀矿化的(构造-地层的、地球化学的、热液交代的等)有利前提是划分此铀矿省的依据。 (2)该铀矿省位于波罗的地盾的东南坡上,并占据着晚太古代克拉通化的卡累利阿巨地块在瑞典-芬兰大地构造旋回中形成的拉多日-勃特纳褶皱系的片段,以及俄罗斯地台与其邻接的部分,上述构造在俄罗斯地台上被文德
(1) After the “Neva State-owned Geological Enterprise”, the All-Russia Institute of Geology and other units for many years of uranium prediction-census specialized work divided the Onega-Radoujon uranium province. The discovery of numerous radioactive geochemical and radiometric anomalies at numerous uranium mines and some small uranium deposits and large-scale integrated uranium-vanadium deposits as well as the discovery of uranium mineralization (tectono-stratigraphic, geochemical, hydrothermal, etc.) The favorable premises is the basis for the division of this uranium province. (2) This uranium province is located on the southeast slope of the Baltic Shield and occupies the Rado-Bertel formed during the structural rotation of the Swedish-Finnish Karelian huge block of the late Archean cratonic Fold wrinkle lines, as well as the Russian platform and its adjacent parts, the above structure on the Russian platform was Wende