Journal ArticleDOI
Post-oxide phases of forsterite and enstatite
TLDR
In this article, the lattice parameters for the perovskite phase of MgSiO3 are ao = 4.790 ± 0.002, bo = 4,943 ± 0.,002, and co = 6.897 ± 0,003 A with Z= 4.083 g/cm³, or 2.8% denser than its isochemical mixed oxides with rocksalt and rutile structures.Abstract:
Both forsterite (Mg2SiO4) and enstatite (MgSiO3) enter a post-oxide phase characterized by the orthorhombic perovskite structure when subjected to high pressure and temperature in the diamond-anvil press coupled with laser heating. The lattice parameters for the perovskite phase of MgSiO3 are ao = 4.790 ± 0.002, bo = 4.943 ± 0.002, and co = 6.897 ± 0.003 A with Z = 4. The calculated density of MgSiO3 (perovskite) is thus 4.083 g/cm³, or 2.8% denser than its isochemical mixed oxides with rocksalt and rutile structures. The density of a mixture of MgSiO3 (perovskite) plus MgO (periclase) is 1.9% greater than that of the mixed oxides with the forsterite stoichiometry.read more
Citations
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Phase transformations and their bearing on the constitution and dynamics of the mantle
TL;DR: The bulk chemical composition of pyrolite is derived from experimental and petrological studies of the complementary relationships between basaltic magmas and refractory peridotites as discussed by the authors.
Journal ArticleDOI
Electronic transitions in perovskite: possible nonconvecting layers in the lower mantle.
TL;DR: The proportion of iron in the low spin state grows with depth, increasing the transparency of the mantle in the infrared region, with a maximum at pressures consistent with the D″ layer above the core-mantle boundary, which suggests the existence of nonconvecting layers in the lowermost mantle.
Journal ArticleDOI
Pyroxene-garnet solid-solution equilibria in the systems Mg4Si4O12Mg3Al2Si3O12 and Fe4Si4O12Fe3Al2Si3O12 at high pressures and temperatures
Masaki Akaogi,Syun-iti Akimoto +1 more
TL;DR: In this article, a pyroxene-garnet solid-solution equilibria have been studied in the pressure range 41-200 kbar and over the temperature range 850-1,450°C for the system Mg4SiO3 in pyrope (Mg3Al2Si3O12), and in a pressure range 30-105 kbar, and over a temperature range 1,000 -1,300
Journal ArticleDOI
Effect of pressure, temperature, and composition on lattice parameters and density of (Fe,Mg)SiO3-perovskites to 30 GPa
Ho-kwang Mao,Russell J. Hemley,Yingwei Fei,Jinfu Shu,L. C. Chen,Andrew P. Jephcoat,Y. Wu,William A. Bassett +7 more
TL;DR: In this paper, the first direct measurements of unit cell distortions and equation-of-state parameters of the orthorhombic perovskite as functions of composition and simultaneous high pressure and high temperature were obtained.
References
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Journal ArticleDOI
The Elastic Behaviour of a Crystalline Aggregate
TL;DR: The connection between the elastic behavior of an aggregate and a single crystal is considered in this article, with special reference to the theories of Voigt, Reuss, and Huber and Schmid.
Journal ArticleDOI
A variational approach to the theory of the elastic behaviour of multiphase materials
Zvi Hashin,S. Shtrikman +1 more
TL;DR: In this paper, the authors derived upper and lower bounds for the effective elastic moduli of quasi-isotropic and quasi-homogeneous multiphase materials of arbitrary phase geometry.
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Finite Elastic Strain of Cubic Crystals
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Journal ArticleDOI
A simplified method for calculating the debye temperature from elastic constants
TL;DR: In this article, it was shown that the Reuss and Voigt approximations can be used to estimate, accurately, the mean sound velocity of a crystal, which is proportioned to the Debye temperature.
Journal ArticleDOI
The velocity of compressional waves in rocks to 10 kilobars: 1.
TL;DR: The velocity of compressional waves has been determined by measurement of travel time of pulses in specimens of rock at pressures to 10 kilobars and room temperature as mentioned in this paper, mainly igneous and metamorphic rocks, furnished three specimens oriented at right angles to one another.
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