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Noble gases (Ar, Kr, Xe) and halogens (Cl, Br, I) in fluid inclusions from the Athabasca Basin (Canada): Implications for unconformity-related U deposits

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Richard, Antonin
Kendrick, Mark
Cathelineau, Michel

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Elsevier

Abstract

The formation of unconformity-related uranium deposits in the Proterozoic Athabasca Basin (Canada) involved basin-scale circulation of U-bearing brines during high-grade diagenesis (150-200°C) at ~1.6-1.5Ga. The UO2 ores occur both sides of the unconform

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Precambrian Research

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Open Access
Open Access

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