Hugoniot equation of state of periclase to 200 GPa

Geophysical Research Letters

Volumn 8, Issue 7, 1981, Pages 729-732

  Vassiliou, M S ^a   Ahrens, Thomas J ^a  

^a NONE

Author keywords

[No Author keywords available]

Indexed keywords

LOWER MANTLE; MAGNESIOWUSTITE; PERICLASE; SHOCK WAVE DATA; SINGLE CRYSTAL;

EID: 0019379285     PISSN: 00948276     EISSN: 19448007     Source Type: Journal    
DOI: 10.1029/GL008i007p00729     Document Type: Article

References (24)

1. Elasticity and Constitution of the Earth's Interior
2. The Pressure and Temperature Dependence of the Elastic Properties of Polycrystal Magnesiowustite
3. The Equation of State of Selected Materials for High Pressure Reference
4. Quasi‐Harmonic Finite Strain Equations of State of Solids
5. Prediction of High Pressure Phase Transitions by Elastic Constant Data
6. The Hugoniot Equation of State of Sodium Chloride in the Sodium Chloride Structure
7. Shock Wave Compression of Single Crystal Forsterite
8. The Elasticity of Periclase to 3 GPa and Some Geophysical Implications
9. Phase Transitions in Rutile‐Type Structures
10. Properties of Iron at High Pressures and the State of the Core
11. Pyroxenes and Olivines: Structural Implications of Shock Wave Data for High Pressure Phases
12. Equations of State of FeO and CaO
13. Anorthite: Thermal Equation of State to High Pressures
14. Phase Transformations and the Constitution of the Deep Mantle
15. Equations of State of MgO and ∈ Fe Under Static Pressure Conditions
16. The Equation of State of Solids from Shock Wave Studies
17. Equation of State of Poly crystalline and Single Crystal MgO to 8 Kilobars and 800°K