
Enstatite - Wikipedia
Enstatite is a mineral; the magnesium endmember of the pyroxene silicate mineral series enstatite (MgSiO 3) – ferrosilite (FeSiO 3). The magnesium rich members of the solid solution series are common rock-forming minerals found in igneous and metamorphic rocks. The intermediate composition, (Mg,Fe)SiO.
Melting and density of MgSiO3 determined by shock …
Feb 9, 2021 · Here, we report an unprecedently high melting temperature of MgSiO3 at 500 GPa by direct shockwave loading of pre-synthesized dense MgSiO3 (bridgmanite) using the Z Pulsed Power Facility.
Post-perovskite - Wikipedia
Post-perovskite (pPv) is a high-pressure phase of magnesium silicate (MgSiO 3). It is composed of the prime oxide constituents of the Earth's rocky mantle (MgO and SiO 2), and its pressure and temperature for stability imply that it is likely to occur in portions of the lowermost few hundred km of Earth's mantle.
Post-Perovskite Phase Transition in MgSiO3 | Science - AAAS
Results demonstrate that MgSiO 3 perovskite transforms to a new high-pressure form with stacked SiO 6 -octahedral sheet structure above 125 gigapascals and 2500 kelvin (2700-kilometer depth near the base of the mantle) with an increase in density of 1.0 to 1.2%.
The MgSiO3 system at high pressure: Thermodynamic properties …
Jan 14, 2009 · We present new equation-of-state (EoS) data acquired by shock loading to pressures up to 245 GPa on both low-density samples (MgSiO3 glass) and high-density, polycrystalline aggregates (MgSiO3 perovs...
Structure, thermodynamic and transport properties of liquid MgSiO3 …
Mar 1, 2011 · Liquid MgSiO 3 is a model for the Earth’s magma ocean and of remnant melt present near the core–mantle boundary.
Structure and Freezing of MgSiO3 Liquid in Earth's Lower Mantle
Oct 14, 2005 · Here, we present FPMD simulations of MgSiO 3 liquid over the pressure-temperature range of Earth's mantle, based on density functional theory in the local density approximation and the plane-wave pseudopotential method (4). The simulations are performed in the canonical ensemble with periodic boundary conditions and a Nosé thermostat (5).
Experimental and theoretical thermal equations of state of MgSiO3 …
Mar 7, 2016 · The MgSiO 3 post-perovskite phase is the most abundant silicate phase in a super-Earth’s mantle, although it only exists within the Earth’s lowermost mantle.
Thermodynamics of Liquid MgSiO3 at High Pressure and …
We use density functional theory molecular dynamics (DFT-MD) and path integral Monte Carlo (PIMC) simulations to generate a consistent equation of state (EOS) for liquid MgSiO3 that spans across a wide range of temperatures and pressures.
Theoretical and experimental evidence for a post-perovskite …
Jul 22, 2004 · Here, using ab initio simulations and high-pressure experiments, we show that at pressures and temperatures of the D″ layer, MgSiO 3 transforms from perovskite into a layered CaIrO 3 -type...