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Scientific Reports|September 6, 2017
Highly oxidising fluids generated during serpentinite breakdown in subduction zonesB Debret, D A SverjenskyGeochimica Et Cosmochimica Acta|April 1, 1997
Prediction of the thermodynamic properties of aqueous metal complexes to 1000 degrees C and 5 kbD A Sverjensky, E L Shock, H C HelgesonGeochimica Et Cosmochimica Acta|March 1, 1997
Inorganic species in geologic fluids: correlations among standard molal thermodynamic properties of aqueous ions and hydroxide complexesE L Shock, D C Sassani, M Willis, et al.Nature Communications|August 8, 2020
Subduction hides high-pressure sources of energy that may feed the deep subsurface biosphereA Vitale Brovarone, D A Sverjensky, F Piccoli, et al.Nature Communications|September 22, 2017
Silicate dissolution boosts the CO<sub>2</sub> concentrations in subduction fluidsS Tumiati, C Tiraboschi, D A Sverjensky, et al.Nature Communications|January 15, 2022
Decoupling of inorganic and organic carbon during slab mantle devolatilisationP Bouilhol, B Debret, E C Inglis, et al.Nature Communications|May 25, 2022
Subducted organic matter buffered by marine carbonate rules the carbon isotopic signature of arc emissionsS Tumiati, S Recchia, L Remusat, et al.Pageof 1