High-Pressure Study of Perovskites and Postperovskites in the (Mg,Fe)GeO₃ System

The effect of incorporation of Fe²⁺ on the perovskite (<i>Pbnm</i>) and postperovskite (<i>Cmcm</i>) structures was investigated in the (Mg,Fe)­GeO₃ system at high pressures and temperatures using laser-heated diamond anvil cell and synchrotron X-ray diffraction. Samples with compositions of Mg# ≥ 48 were shown to transform to the perovskite (∼30 GPa and ∼1500 K) and postperovskite (>55 GPa, ∼1600–1800 K) structures. Compositions with Mg# ≥ 78 formed single-phase perovskite and postperovskite, whereas those with Mg# < 78 showed evidence for partial decomposition. The incorporation of Fe into the perovskite structure causes a decrease in octahedral distortion as well as a modest decrease in bulk modulus (<i>K</i>₀) and a modest increase in zero-pressure volume (<i>V</i>₀). It also leads to a decrease in the perovskite-to-postperovskite phase transition pressure by ∼9.5 GPa over compositions from Mg#78 to Mg#100