Castelli, D.

Ferrando, S.

Maffeis, A.

English

Institutional Research Information System University of Turin

P-T-fO2 C and S speciation in subduction zone fluids as obtained by electrolytic-fluid thermodynamic modelling of impure carbonate system A. Maffeis1, J. A.D. Connolly2, M.L. Frezzotti3, D. Castelli1, S. Ferrando1 1 Università degli Studi di Torino, Dipartimento di Scienze della Terra, Torino, Italy; 2 ETH Zurich, Department of Earth Sciences, Institute for Geochemistry and Petrology, Zurich, Switzerland 3 Università degli Studi di Milano-Bicocca, Dipartimento di Scienze dell’Ambiente e della Terra  Element speciation in subduction fluids controls the transport efficiency of elements from the down-going slab to the overlying mantle wedge. Elemental speciation is controlled by PTfO2 and bulk-rock composition (i.e., rock-buffered). Elements like C and S are characterised by a wide range of possible valance states, making them crucial in regulating the redox state of the arc mantle and the associated volcanism. However, dominant carbonate sediments (representing ~70% of the total subducted carbon; Clift, 2017) are only marginally considered in the modelled subduction processes, mostly because of the lack of relevant decarbonation reactions at HP-UHP conditions. Similarly, because S is considered to be primarily subducted at UHP conditions as sulphides or sulphates within the altered oceanic crust (e.g., Walters et al., 2020), the S input from dominant carbonate sediments has been rarely considered. To address the role of dominant carbonate sediments on the C and S long term cycles, we conducted electrolytic-fluid thermodynamic modelling of the fluid phase in equilibrium with a UHP impure marble from the Dora-Maira Massif (Western Alps). This marble experienced multiple carbonated dissolution-precipitation events during active subduction at HP-UHP conditions. The study of this natural sample allows linking the thermodynamically modelled HP-UHP evolution, of both rock and fluid, to the HP-UHP mineral assemblages and related fluid inclusions (Maffeis et al., 2021). Using the bulk composition of the studied marble, we modelled the chemical evolution of the fluid along the prograde P-T path (from ~490°C-1.5 GPa to ~730°C-4.3 GPa) and of at different fO2 (between +2 and -2 from the FMQ buffer). At changing P-T-fO2 conditions, C and S speciation and concentration in the fluid are different. At reduced conditions, C is additionally speciated as carboxylic compounds and hydrocarbons, while S is speciated as H2S and HS-. At oxidized conditions, C and S are speciated as HCO3- and SO42-, respectively. The dissolution of carbonate dominated sediments is an effective process for the mobilisation of both C and S, with C being more easily released at reduced conditions and S at oxidised conditions instead. Thus, dissolution is a more effective process than decarbonation and desulphurisation reactions in releasing C and S during subduction at sub-arc depths. Clift, P. D. 2017. A revised budget for Cenozoic sedimentary carbon subduction. Reviews of Geophysics, 55(1), 97-125. Maffeis, A., Ferrando, S., Connolly, J. A., Groppo, C., Frezzotti, M. L., & Castelli, D. 2021. Thermodynamic analysis of HP-UHP fluid inclusions: The solute load and chemistry of metamorphic fluids. Geochimica et Cosmochimica Acta, 315, 207-229. Walters, J. B., Cruz-Uribe, A. M., & Marschall, H. R. 2020. Sulfur loss from subducted altered oceanic crust and implications for mantle oxidation. Geochemical Perspectives Letters, 13, 36-41. 

P-T-fO2 C and S speciation in subduction zone fluids as obtained by electrolytic-fluid thermodynamic modelling of impure carbonate system

https://iris.unito.it/bitstream/2318/1891131/1/Maffeis_IEC_14_COHS_Fluid.pdf

P-T-fO2 C and S speciation in subduction zone fluids as obtained by electrolytic-fluid thermodynamic modelling of impure carbonate system

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