At the Rabbit Lake uranium deposit, uranium occurs in several generations of pitchblende and in diverse secondary radioactive minerals that are characterized by marked differences in the content of radiogenic lead. The isotopic studies were undertaken to attempt to date the major events in the complex history of this deposit. these include periods of remobilization of the uranium and radiogenic lead, the emplacement of sulphides (including selenides and arsenides), silicification, oxidation, argillization, and carbonatization, as well as the time of original emplacement of the pitchblende.