The relationship between Δ30 and N2/3He ratios in hydrothermal gases from
The relationship between Δ30 and N2/3He ratios in hydrothermal gases fromThe relationship between Δ30 and N2/3He ratios in hydrothermal gases from Iceland and Yellowstone. Δ30 and N2/3He ratios are shown for samples collected from gases in Iceland (yellow circles) and Yellowstone (red circles). The Yellowstone mantle-endmember is arguably indistinguishable in terms of N2/3He from the convecting upper mantle (grey diamonds).