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- W2035201483 abstract "A thermodynamic method in which all physical properties (derivatives of the Helmholtz energy) are determined from seven thermoelastic parameters is used to calculate density isentropes of (Mg,Fe)SiO 3 perovskite for lower mantle conditions. We find that, provided the EoS constants, ρ 0 , K To , and K' 0 , are known, the density distribution can be found from the thermal pressure and often from the thermal pressure evaluated at zero pressure. Three isentropic density distributions of perovskite are calculated and are shown to be non-parallel with PREM's density distribution. This leads to the speculation that a lower mantle entirely composed of perovskite may not be phase homogeneous throughout its whole depth." @default.
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- W2035201483 date "1995-08-15" @default.
- W2035201483 modified "2023-09-26" @default.
- W2035201483 title "The isentropic density profile of silicate perovskite computed by the thermal pressure" @default.
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- W2035201483 doi "https://doi.org/10.1029/95gl01726" @default.
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