Constitution of the Moon: 2. Composition and seismic properties of the lower mantle

Physics of the Earth and Planetary Interiors

Volumn 83, Issue 3-4, 1994, Pages 197-216

  Kuskov, O L ^a   Fabrichnaya, O B ^a  

^a UPPSALA UNIVERSITY   (Sweden)

Author keywords

[No Author keywords available]

Indexed keywords

LUNAR MANTLE; MINERALOGY; PHASE ROTATION; THERMODYNAMICS;

EID: 0028193704     PISSN: 00319201     EISSN: None     Source Type: Journal    
DOI: 10.1016/0031-9201(94)90089-2     Document Type: Article

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6. Single-crystal X-ray structure study of synthetic pyrope almandine garnets at 100 and 293 K
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9. Elasticity of grossular and spessartite garnets by Brillouin spectroscopy
10. Elasticity of single-crystal orthoferrosilite
11. Mixing properties of CaMgFeMn garnets
12. An improved set of a-X parameters for FeMgCa garnets and refinements of the orthopyroxene-garnet thermometer and the orthopyroxene-garnet-plagioclase-quartz barometer
13. Olivine-spinel transitions: Experimental and thermodynamic constraints and implications for the nature of the 400-km seismic discontinuity
14. The pressure and temperature dependence of the elastic constants of pyrope garnet
15. Structure of the upper mantle beneath Lesotho
16. The impact theory for the origin of the Moon
17. The computation of equilibrium in complex systems containing non-ideal solutions
18. Pressure dependence of single-crystal elastic constants and anharmonic properties of spinel
19. Sound velocities of MgO to very high compression and d ln γ/d ln V in the lower mantle
20. General relationship among sound speeds
21. Thermal expansion of stishovite at 98–420 K
22. Thermal expansion in the pyrope-grossular and pyrope-knorringite garnet series
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24. Seismic velocities in mantle minerals and the minerology of the upper mantle
25. Preliminary reference Earth model
26. Constitution of the mantle
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44. Erratum
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46. CODATA International Geothermodynamic Tables
47. The competition between thermal contraction and differentiation in the stress history of the Moon
48. Solution properties of almandine-pyrope garnet as determined by phase equilibrium experiments
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56. Construction of thermal equations of state for periclase, coesite, and stishovite from the bulk moduli and calculation of the coesite-stishovite phase equilibrium
57. The reliability of thermodynamic calculations on chemical and phase equilibria at ultrahigh pressures
58. 2 system at P-T parameters of the mantle transition zone
59. Thermodynamics of silica polymorphism
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62. High-pressure crystal structure and compressibility of coesite
63. Compression of pyrope
64. Elasticity of pyroxene-garnet and pyroxene-ilmenite phase transformations in germanates
65. Elastic properties of anorthite and the nature of the lunar crust
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69. Elastic properties of pyrope
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76. Hydrostatic compression of the synthetic garnets pyrope and almandine
77. Planetary phase equilibria: application to formation of Earth, Venus and Mercury
78. 2
79. Theoretical computation of mineral assemblages in pyrolite and lherzolite
80. Chemistry of the formation of the terrestrial planets
81. Assessed data on heat capacity, thermal expansion, and compressibility for some oxides and silicates
82. Thermal expansivity of ten minerals
83. Lunar Electrical Conductivity Profile
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85. The crystal structure of stishovite under pressure up to 6GPa.
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87. Temperature coefficients of elastic constants of single crystal MgO between 80 and 1300 K
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90. 4
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97. Linear Thermal Expansion of Aluminum Oxide and Thorium Oxide from 100o to 1100oK
98. Elasticity of some mantle crystal structures
99. Elasticity of some mantle crystal structures
100. The bulk-moon MgO/FeO ratio: a highlands perspective
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102. Comparison between thermochemical and phase stability data for the quartz-coesite-stishovite transformations
103. Elasticity of coesite
104. Elasticity of orthoenstatite
105. The single-crystal elastic moduli of stishovite
106. 3
107. 4
108. Fluid phases and the redox state of the Earth's mantle
109. Theoretical prediction of phase relationships in planetary mantles
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111. 4
112. Compression of synthetic pyrope up to 10 Gpa