Data for: Self-diffusion and chemical diffusion in peridotite melt at high pressure and implications for magma ocean viscosities

Published: 17-11-2018| Version 1 | DOI: 10.17632/6zrzwm3yxb.1
Esther Posner


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.