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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文摘

Brines involved in Proterozoic U deposits (Athabasca, Canada) are targeted.

Halogens (Cl, Br, I) indicate a subaerial evaporation of seawater origin for brines.

Brines acquired excess noble gases (Ar, Kr, Xe) by interaction with clastic sediments.

Interaction with basement-derived fluid or organic matter is unlikely.

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