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We investigate the effect of solute drag on grain growth (GG) kinetics inolivine-rich rocks through full field and mean field modelling. Considering adrag force exerted by impurities on grain boundary migration allows reconcilinglaboratory and natural constraints on olivine GG kinetics. Solute drag isimplemented in a full field level-set framework and on a mean field model,which explicitly accounts for a grain size distribution. After calibration ofthe mean field model on full field results, both models are able to bothreproduce laboratory GG kinetics and to predict grain sizes consistent withobservations in peridotite xenoliths from different geological contexts.

On the role of solute drag in reconciling laboratory and natural constraints on olivine grain growth kinetics