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Magnesite (MgCO 3 ) is an important phase for the carbon cycle in and out of the Earth’s mantle. Its comparably large P-T stability has been inferred for several years based on the absence of its decomposition in experiments. Here we report the first experimental evidence for synthesis of magnesite out of its oxide components (MgO and CO 2 ) at P-T conditions relevant to the Earth’s mantle.

Magnesite formation from MgO and CO 2 at the pressures and temperatures of Earth’s mantle