Abstract
High-pressure phase stabilities of the CaSnO3 system were investigated using density functional theory static lattice energy calculations. We have identified six phase changes in this system: perovskitepost-perovskite, post-perovskite-B2+cotunnite in CaSiO3, B1-B2 in CaO, cassiterite-pyrite, pyriteorthorhombic-I, and orthorhombic-I-cotunnite in SnO2. Our results demonstrate a new high-pressure phase sequence of perovskite → post-perovskite → B2 + cotunnite. The post-perovskite transformation occurs at ~12 GPa with ~2.5% volume reduction and then it decomposes into the oxide mixture of B2 CaO and cotunnite SnO2 at ~70 GPa with 8.1% volume reduction. The results also predict a few percent bulk velocity variations across these phase changes.
© 2015 by Walter de Gruyter Berlin/Boston
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Articles in the same Issue
- Presidential Address to the Mineralogical Society of America, Salt Lake City, October 18, 2005: Mineral surfaces and the prebiotic selection and organization of biomolecules
- A rare garnet-tourmaline-sillimanite-biotite-ilmenite-quartz assemblage from the granulite-facies region of south-central Massachusetts
- Effects of natural radiation damage on back-scattered electron images of single crystals of minerals
- Thermal diffusivity of olivine-group minerals at high temperature
- Quantum mechanical vs. empirical potential modeling of uranium dioxide (UO2) surfaces: (111), (110), and (100)
- AXANES study of Cu speciation in high-temperature brines using synthetic fluid inclusions
- A new approach to determine and quantify structural units in silicate glasses using micro-reflectance Fourier-Transform infrared spectroscopy
- Titanium incorporation and VITi3+ -IVTi4+ charge transfer in synthetic diopside
- Hugoniot and impact-induced phase transition of magnesite
- Finite element modeling of elastic volume changes in fluid inclusions: Comparison with experiment
- Thermodynamics of mixing in pyrope-grossular, Mg3Al2Si3O12-Ca3Al2Si3O12, solid solution from lattice dynamics calculations and Monte Carlo simulations
- Does antigorite really contain 4- and 8-membered rings of tetrahedra?
- New insight into crystal chemistry of topaz: A multi-methodological study
- Tetrahedrally coordinated boron in tourmalines from the liddicoatite-elbaite series from Madagascar: Structure, chemistry, and infrared spectroscopic studies
- Recovery of stishovite-structure at ambient conditions out of shock-generated amorphous silica
- New experimental data on biotite + magnetite + sanidine saturated phonolitic melts and application to the estimation of magmatic water fugacity
- Structural effects of pressure on triclinic chlorite: A single-crystal study
- New high-pressure phase relations in CaSnO3
- A high-pressure Raman spectroscopic study of hafnon, HfSiO4
- Single-crystal elasticity of brucite, Mg(OH)2, to 15 GPa by Brillouin scattering
- The effect of composition on Cr2+/Cr3+ in silicate melts
- Phosphohedyphane, Ca2Pb3(PO4)3Cl, the phosphate analog of hedyphane: Description and crystal structure
- Synthesis of novel leadmolybdenum and leadtungsten oxyhalides with the pinalite structure, Pb3MoO5Cl2 and Pb3WO5Br2
- Depolymerization effect of water in aluminosilicate glasses: Direct evidence from 1H-27Al heteronuclear correlation NMR
- Hydroxylellestadite from Cioclovina Cave (Romania): Microanalytical, structural, and vibrational spectroscopy data
- Matioliite, the Mg-analog of burangaite, from Gentil mine, Mendes Pimentel, Minas Gerais, Brazil, and other occurrences
- Letter. Crystallographic alignments in a coccolith (Pleurochrysis carterae) revealed by electron back-scattered diffraction (EBSD)
- Letter. High-pressure study of FeS, between 20 and 120 GPa, using synchrotron X-ray powder diffraction