Data for: Self-diffusion and chemical diffusion in peridotite melt at high pressure and implications for magma ocean viscosities
Published: 17 November 2018| Version 1 | DOI: 10.17632/6zrzwm3yxb.1
The attached spreadsheet contains pre-exponential diffusion coefficients fitted using fixed activation enthalpies of 100, 200, or 300 kJ/mol to isotopic (Si, O, Mg, Ca) or compositional (Ni, Co) profiles developed during diffusion experiments in peridotite melt at high pressure. For more information, please see the manuscript.
Geochemistry, Petrology, Diffusion, Magma, Experimental Geochemistry, Experimental Petrology, Silicate Melt