Fig. 5: Global ionic mass fluxes. | Nature Communications

Fig. 5: Global ionic mass fluxes.

From: Large-scale groundwater flow and sedimentary diagenesis in continental shelves influence marine chemical budgets

Fig. 5

a Fluxes from mid-ocean ridge (MOR) hydrothermal convection and for the four fluid archetypes as trial fluxes from passive continental margins. b Minimum theoretical mass fluxes (Cth, Eq. 1) required to close chemical budgets if low-temperature basalt alteration is not considered. Source data are provided as a Source Data file.

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