Extended Data Fig. 2: CO2 flux population analyses.
From: Displaced cratonic mantle concentrates deep carbon during continental rifting
a–d, Shown are results for the Manyara (a), Natron (b), Magadi (c) and Balangida (d) basins. The analyses were performed in line with the method of Sinclair67 outlined in Chiodini et al.65, with the dashed lines representing a modelled mixed population based on the distributions of the lower, higher and occasionally intermediate flux populations.
