Quantitative spectrographic analyses for Cr, V, Cu, Ni, and Co of 219 specimens of the country rocks from the Beaverlodge area, Saskatchewan, and chemical analyses for U of 68 of those rock specimens and for Th of 38 of them have shown that positive relationships exist between the above elements and uranium in quartzite, and that quartzite may be the principal source of uranium in the uranium deposits.

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