Using aqueous silica activity to model ƒO2 in the serpentinized forearc mantle: implications for redox-sensitive fluid speciation from 1-20 kbar and 100-700°C
Using aqueous silica activity to model ƒO2 in the serpentinized forearc mantle: implications for redox-sensitive fluid speciation from 1-20 kbar and 100-700°C