Experimental determination of compressional wave velocities of olivine aggregate up to 1000°C at 1 GPa

Tectonophysics

Volumn 339, Issue 3-4, 2001, Pages 473-478

  Aizawa, Yoshitaka ^a   Ito, Kazuhiko ^b   Tatsumi, Yoshiyuki ^a,c  

^a KYOTO UNIVERSITY   (Japan)

^b Southern Osaka University   (Japan)

^c JAPAN AGENCY FOR MARINE EARTH SCIENCE AND TECHNOLOGY   (Japan)

Author keywords

Compressional wave velocity; High pressure; High temperature; Olivine aggregate

Indexed keywords

HIGH PRESSURE; HIGH TEMPERATURE; OLIVINE; P-T CONDITIONS; S-WAVE; SEISMIC VELOCITY;

EID: 0035203283     PISSN: 00401951     EISSN: None     Source Type: Journal    
DOI: 10.1016/S0040-1951(01)00133-0     Document Type: Article

References (21)

1. Compressional wave velocity in rocks at high temperatures and pressures, critical thermal gradients, and crustal low velocity zones
2. Seismic velocities in mantle minerals and the mineralogy of the upper mantle
3. The high-low quartz transition up to 10 kbars pressure
4. Crustal layers of the continents and oceans
5. High temperature elasticity of iron-bearing olivines
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7. Seismic wave dispersion and attenuation in Åheim dunite
8. Importance of physical dispersion in surface- wave and free-oscillation problems, review
9. Importance of anelasticity in the interpretation of seismic tomography
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12. Elastic moduli, pressure derivatives and temperature derivatives of single-crystal olivine and single crystal forsterite
13. Some remarks on heat flow and gravity anomalies
14. The volume and composition of melt generated by extension of the lithosphere
15. Pressure derivatives of elastic wave velocities from ultrasonic interferometric measurements on jacketed polycrystals
16. Temperature dependence of the compressional wave velocity in isotropic dunite: Measures to 500°C at 10 kbar
17. The use of laboratory velocity data for estimating temperature and partial melt fraction in the low-velocity zone: Comparison with heat flow and electrical conductivity studies
18. Thermal expansion of periclase and olivine, and their anharmonic properties
19. Computation of seismic profiles from mineral physics: The importance of the non-olivine components for explaining the 660 km depth discontinuity
20. The elasticity of the upper mantle orthosilicates olivine and garnet to 3 GPa