The reduction kinetics of oolitic hematite at 1173–1473 K is investigated by the microwave direct reduction. The effects of reduction temperature and time on the reduction of oolitic hematite are investigated in terms of FeO concentration in metalised pellets. The reduced samples are characterised by XRD, SEM and EDS. The results indicate that the degree of carbonisation reduction of iron ore pellets is further increased by the intensification of microwave. The reduction of iron oxide follows the deoxidation process of Fe3+→Fe2+→Fe0, and the FeO concentration gradually reduces and tends to level off with the increase of the reduction degree. Different kinetic models are fitted to the reduction rate to determine that the reduction process conforms to the Ginsley-Brousstein equation, and the limiting link is the gaseous internal diffusion, with an apparent activation energy of 11.535 kJ/mol.