Finding the isentropic density of perovskite: Implications for iron concentration in the lower mantle
Author:
Publisher
American Geophysical Union (AGU)
Subject
General Earth and Planetary Sciences,Geophysics
Link
http://www.agu.org/journals/gl/v024/i003/96GL03951/96GL03951.pdf
Reference14 articles.
1. A thermoelastic method for computing thermal expansivity, α versus T along isobars for silicate perovskite;Anderson;Phys. Earth Planet. Inter.,1994
2. Limits on the value of δT and γ for MgSiO3 perovskite and MgO;Anderson;Phys. Earth Planet. Inter.,1996
3. Thermal expansivity in the lower mantle;Chopelas;Geophys. Res. Lett,1992
4. Thermoelastic properties of MgSiO3 perovskite determined by insitu x-ray observations up to 30 GPa and 2000 K;Funamori;J. Geophys. Res.,1996
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1. A new family of planets? “Ocean-Planets”;Icarus;2004-06
2. Constraints on lower mantle composition from molecular dynamics simulations of MgSiO3 perovskite;Physics of the Earth and Planetary Interiors;2002-12
3. Computational mineral physics and the physical properties of perovskite;Philosophical Transactions of the Royal Society of London. Series A: Mathematical, Physical and Engineering Sciences;2002-09-27
4. High-pressure sound velocity of perovskite-enstatite and the possible composition of the Earth’s lower mantle;Chinese Science Bulletin;2000-05
5. High-Pressure Sound Velocity of Perovskite-Enstatite and Possible Composition of Earth's Lower Mantle;Chinese Physics Letters;1999-09-01
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