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The concordance of the noble gas systems, and other multiple lines of proof (e.g. δ18O, δ2H, sulfur isotopes)two,19, demonstrated the Kidd Creek fracture network was an example of extended hydrogeologic isolation of fluids. On the other end of the open-closed spectrum, some deep crustal environments are impacted by the penetration of surface-derived paleometeoric water with residence times in the ka-Ma range to depths of much more than 1 km16,17. Adding to this disruption, rates for the supply of...
