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Source of Uranium (U) and Rare Earth Elements (REE) for Unconformity-Related U and REE Mineralization in the Athabasca Basin, Canada: Insights from Accessory Minerals in Sandstones
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DOI：10.1016/j.apgeochem.2026.106953.png)
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Abstract
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• Detrital zircon and rutile are the dominant U and REE carriers in the Athabasca sandstones • Textural and compositional evidence indicates U and REE were leached from zircon and rutile • The U and REE in the unconformity-related U deposits were mainly derived from the basin • Much more U and REE were released from zircon and rutile than found in the deposits
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