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Am. Mineral. 85, 283-287. , 1979. Growth of wiistite Fei_;,0 crystals of various stoichiometrics. J. Cryst. Growth 47, 736-738. , 1952. Elasticity and constitution of the Earth's interior. J. Geophys. Res. 57, 227-285. , 1982. The pressure and temperature dependence of the elastic properties of polycrystal magnesiowiistite. J. Geophys. Res. 87, 1061-1078. , 1965. Pure modes for elastic waves in crystals. J. Appl. Phys. 36, 759-768. , 1997. The elastic constants of a pyrope-grossular-almandine garnet to 20 GPa.

S. F. V. All rights reserved. 25 Chapter 2 A gigahertz ultrasonic interferometer for the diamond anvil cell and high-pressure elasticity of some iron-oxide minerals Steven D. Jacobsen, Hans J. Reichmann, Anastasia Kantor and Hartmut A. Spetzler Abstract A second-generation high-frequency acoustic interferometer has been developed for high-pressure and high-temperature elasticity measurements in the diamond anvil cell The instrument measures single-crystal compressional and shear-wave travel times, which are converted to sound velocities and elastic moduli for direct application to problems in geophysics.

30, 430-439. , 1989. Measured elastic moduU of single-crystal MgO up to 1800 K. Phys. Chem. Miner. 16, 704-713. , 1996. Pressure effect on the elastic constants of magnetite. Physica B 219-220, 638-640. , 1982. The elasticity of periclase to 3 GPa and some geophysical implications. H. (Eds), High-Pressure Research in Geophysics. , Japan, pp. 93-113. , 1990. Elasticity, shear-mode softening and highpressure polymorphism of wiistite (Fci-vO). J. Geophys. Res. 95, 21671-21685. , 2003. Highpressure Brillouin measurements on single-crystal ferropericlase, (Mgo 94Fe() 06)0: implications for Earth's lower mantle.

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Advances in high-pressure technology for geophysical applications


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