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The cation distribution in magnesioferrite MgFe 2 O 4  was investigated using a “piston-cylinder” apparatus at three pressures (ambient, 1, and 2 GPa) over a temperature range of 600 to 1200 °C. Quenched samples of magnesioferrite were investigated by X-ray powder diffraction. The inversion parameter was derived from the unit-cell parameter at ambient temperature.

Letter. Cation distribution in MgFe 2 O 4 vs. pressure and temperature: Experiments in a piston-cylinder apparatus