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The rheology is crucial for interpretation of a wide range of geodynamic processes,such as the strain localization at plate boundaries,the attenuation of seismic waves,and fluid and melt transport.The electrical conductivity of the partially molten carbonated peridotite was measured in several experiments(Huang et al.,2012).The olivine aggregates with 5wt%sodium carbonate were deformed in a solidmedium apparatus at temperature 1023-1423K and pressure 900-1300MPa in this study.