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Improved post-perovskite structure models of MgGeO3 (Cmcm) are obtained via development of a new graphite gasket for the diamond anvil cell which increases the volume of sample and quality of diffraction data at pressures near 100 GPa. These models agree with a structure survey supporting a new method for estimating the Clapeyron slope between perovskite (Pbnm) and post-perovskite structures of MgSiO3.
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