Hydrothermal isotopes from Yellowstone and Iceland
Detailed Description
The 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). Modified from Labidi et al., 2020.
Sources/Usage
Public Domain.