Comparison between the Au and MgO pressure calibration standards at high temperature

Geophysical Research Letters

Volumn 29, Issue 10, 2002, Pages 6-1-6-4

  Matsui, Masanori ^a   Nishiyama, Norimasa ^b  

^a UNIVERSITY OF HYOGO   (Japan)

^b UNIVERSITY OF TOKYO   (Japan)

Author keywords

[No Author keywords available]

Indexed keywords

CALIBRATION; HIGH TEMPERATURE EFFECTS; MAGNESIA; MOLECULAR DYNAMICS;

INTERATOMIC POTENTIAL;

GEOPHYSICS;

EQUATION OF STATE; GOLD; HIGH PRESSURE; MAGNESIUM;

EID: 0037095933     PISSN: 00948276     EISSN: None     Source Type: Journal    
DOI: 10.1029/2001gl014161     Document Type: Article

References (22)

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3. MgO-The simplest oxide
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5. 4 to 26 GPa and 900 K
6. 3 perovskite determined by in situ X ray observations up to 30 GPa and 2000 K
7. 12: Implications for the nature of the seismic discontinuities in the Earth's mantle
8. The equation of state of platinum to 660 GPa (6.6 Mbar)
9. High pressure effects on thermal properties of MgO
10. 4 determined by in situ X-ray diffraction
11. 4 and some geophysical implications
12. 3 perovskite from calorimetry
13. Pressure measurement at high temperature in X-ray diffraction studies: Gold as a primary standard
14. 3 by in situ X-ray diffraction and quench experiments
15. 3-perovskite to 30 GPa
16. Breathing shell model in molecular dynamics simulation: Application to MgO and CaO
17. The MD simulation of the equation of state of MgO: As a pressure calibration standard at high temperature and high pressure
18. 4 to mantle pressures and 700 K: Thermal equation of state and related thermoelastic properties
19. In situ X-ray observation of spinel-postspinel and majorite-perovskite transitions in a pyrolite composition
20. 3 perovskite in the Earth's lower mantle
21. 4 and its relation to the 660-km seismic discontinuity
22. Quasi-hydrostatic compression of magnesium oxide to 52 GPa: Implications for the pressure-volume-temperature equation of state