Raman spectroscopic study of hydrous γ-Mg2SiO4 to 56.5 GPa

Physics and Chemistry of Minerals

Volumn 29, Issue 7, 2002, Pages 473-476

  Kleppe, A K ^a   Jephcoat, A P ^a   Smyth, J R ^b  

^a UNIVERSITY OF OXFORD   (United Kingdom)

^b UNIVERSITY OF COLORADO   (United States)

Author keywords

Diamond anvil cell; High pressure; Hydrous minerals; Raman spectroscopy; Ringwoodite

Indexed keywords

CRYSTAL CHEMISTRY; CRYSTAL STRUCTURE; DIAMOND ANVIL CELL; HIGH PRESSURE; HYDROUS MINERAL; RAMAN SPECTROSCOPY; RINGWOODITE;

EID: 0036674402     PISSN: 03421791     EISSN: None     Source Type: Journal    
DOI: 10.1007/s00269-002-0255-5     Document Type: Article

References (13)

1. 2O system up to 24 GPa: Implications for the distribution of water in the Earth's mantle
2. 4 phase equilibrium
3. Operation of the megabar diamond-anvil cell
4. 4) to 50 GPa
5. On protons, iron and the high-pressure behavior of ringwoodite
6. 4
7. Structure and cation disorder of hydrous ringwoodite,
8. 3-pervoskite
9. 4 (spinel)
10. 4 to to mantle pressures at 700 K: Thermal equation of state and related thermoelastic properties
11. 3-rich garnet revealed by Raman spectroscopy
12. 4 to 56.5 GPa spectra of spinels
13. Isothermal compressibility of hydrous ringwoodite and its relation to the mantle discontinuities