Sound velocities of wadsleyite β-(Mg0.88Fe0.12)2SiO4 to 10 GPa

American Mineralogist

Volumn 85, Issue 2, 2000, Pages 292-295

  Li, Baosheng ^a   Liebermann, Robert C ^a  

^a STONY BROOK UNIVERSITY   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

ACOUSTIC WAVE VELOCITY; ELASTIC MODULI; SHEAR STRAIN; SILICON; SINGLE CRYSTALS; ULTRASONIC TESTING;

COMPOSITIONAL RANGE; FINITE STRAIN; IRON CONTENT; POLYCRYSTALLINE SPECIMEN; PRESSURE DERIVATIVES; THIRD ORDER; ULTRASONIC TECHNIQUES; WADSLEYITE;

SHEAR FLOW;

OLIVINE; ULTRASONICS; WADSLEYITE;

EID: 0034107526     PISSN: 0003004X     EISSN: None     Source Type: Journal    
DOI: 10.2138/am-2000-2-305     Document Type: Article

References (20)

1. Cook, R.K. (1957) Variation of elastic constants and static strains with hydrostatic pressure: A method for calculation from ultrasonic measurements. Journal of Acoustic Society of America, 29, 445-449.
2. Bina, C.R. and Wood, B.J. (1987) Olivine-spinel transitions: experimental and thermodynamic constraints for the nature of the 400 km seismic discontinuity. Journal of Geophysical Research, 92, 4853-4866.
3. Davies, G.F. and Dziewonski, A.M. (1975) Homogeneity and constitution of the Earth's lower mantle and outer core. Physics of the Earth and Planetary Interiors, 10, 336-343.
4. Duffy, T.S. and Anderson, D.L. (1989) Seismic velocities in mantle minerals and the mineralogy of the upper mantle. Journal of Geophysical Research, 94, 1895-1912.
5. 4 to 26 GPa and 900 K. Journal of Geophysical Research, 97, 4489-4495.
6. Gwanmesia, G.D. and Liebermann, R.C. (1992) Polycrystals of high-pressure phases of mantle minerals: Hot-pressing and characterization of physical properties. In Y. Syono and M. Manghnani, Ed., High Pressure Research: Application to Earth and Planetary Sciences. American Geophysical Union, Washington, D.C.
7. 4 and the composition of the Earth's mantle. Science, 250, 794-797.
8. Jackson, I., Niesler, H., and Weidner, D.J. (1981) Explicit correction of ultrasonically determined elastic wave velocities for transducer-bond phase shift. Journal of Geophysical Research, 86, 3736-3748.
9. 4 at high pressures and temperatures: precise determination of stabilities of olivine, modified spinel and spinel. Jounral of Geophysical Research, 94, 15663-15670.
10. Li, B., Chen, G., Gwanmesia, G.D., and Liebermann, R.C. (1998a) Sound velocity measurements at mantle transition zone conditions of pressure and temperature using ultrasonic interferometry in a multi-anvil apparatus. In M. H. Manghnani and Y. Syono, Ed., Properties of Earth and Planetary Material at High Pressure and Temperature, 562 p. American Geophysical Union, Washington, D.C.
11. 4) to 7 gigapascals and 873 kelvin. Science, 281, 675-677.
12. Li, B., Jackson, I., Gasparik, T., and Liebermann, R.C. (1996a) Elastic wave velocity measurement in multi-anvil apparatus to 10 GPa using ultrasonic interferometry. Physics of the Earth and Planetary Interiors, 98, 79-91.
13. 4 at Earth's transition zone pressures. Geophysical Research Letters, 23, 2259-2262.
14. 4. Journal of Geophysical Research, 98, 23199-23207.
15. 4 determined by in situ X-ray observation. Science, 265, 1202-1203.
16. Niesler, H. and Jackson, I. (1989) Pressure derivatives of elastic wave velocities from ultrasonic interferometric measurements on jacketed polycrystals. Journal of the Acoustical Socieity of America, 86, 1573-1585.
17. Sawamoto, H., Weidner, D.J., Sasaki, S., and Kumazawa, M. (1984) Single-crystal elastic properties of the modified-spinel (beta) phase of magnesium orthosilicate. Science, 224, 749-751.
18. Sinogeikin, S.V., Bass, J.D., and Katsura, T. (1998), Sound velocity and elastic properties of Fe-bearing wadsleyite and ringwoodite. Journal of Geophysical Research, 103, 20819-20825.
19. Weidner, D.J. (1985) A mineral physics test of a pyrolite mantle. Geophysical Research Letters, 12, 417-420.
20. 4 polymorphs at high pressure. In M.H. Manghnani and Y. Syono, Ed., Properties of Earth and Planetary Material at High Pressure and Temperature. 562 p. American Geophysical Union, Washington, D.C.