Noble gases (Ar, Kr, Xe) and halogens (Cl, Br, I) in fluid inclusions from the Athabasca Basin (Canada): Implications for unconformity-related U deposits
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
|Collections||ANU Research Publications|
|01_Richard_Noble_gases_(Ar,_Kr,_Xe)_and_2014.pdf||1.94 MB||Adobe PDF||Request a copy|
Items in Open Research are protected by copyright, with all rights reserved, unless otherwise indicated.