Iron silicate perovskite and postperovskite in the deep lower mantle

Abstract

Ferromagnesian silicates are the dominant constituents of the Earth’s mantle, which comprise more than 80% of our planet by volume. To interpret the low shear-velocity anomalies in the lower mantle, we need to construct a reliable transformation diagram of ferromagnesian silicates over a wide pressure–temperature ( P-T ) range. While MgSiO 3 in the perovskite structure has been extensively studied due to its dominance on Earth, phase transformations of iron silicates under the lower mantle conditions remain unresolved. In this study, we have obtained an iron silicate phase in the perovskite (Pv) structure using synthetic fayalite (Fe 2 SiO 4 ) as the starting material under P-T conditions of the lower mantle. Chemical analyses revealed an unexpectedly high Fe/Si ratio of 1.72(3) for the Pv phase in coexistence with metallic iron particles, indicating incorporation of about 25 mol% Fe 2 O 3 in the Pv phase with an approximate chemical formula (Fe 2+ 0.75 Fe 3+ 0.25 )(Fe 3+ 0.25 Si 0.75 )O 3 . We further obtained an iron silicate phase in the postperovskite (PPv) structure above 95 GPa. The calculated curves of compressional ( V P ) and shear velocity ( V S ) of iron silicate Pv and PPv as a function of pressure are nearly parallel to those of MgSiO 3 , respectively. To the best of our knowledge, the iron silicate Pv and PPv are the densest phases among all the reported silicates stable at P-T conditions of the lower mantle. The high ferric iron content in the silicate phase and the spin-crossover of ferric iron at the Si-site above ~55 GPa should be taken into account in order to interpret the seismic observations. Our results would provide crucial information for constraining the geophysical and geochemical models of the lower mantle.