Mantle and Core in Planetary Physics, Volume 50Michele Caputo, Jean Coulomb |
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Page 117
... solid rather than liquid medium ; the limiting pressure is then determined by the flow properties of this solid . ) The tangential stress problem is avoided by clever geometries , typically involving cutting the cylinder so that one has ...
... solid rather than liquid medium ; the limiting pressure is then determined by the flow properties of this solid . ) The tangential stress problem is avoided by clever geometries , typically involving cutting the cylinder so that one has ...
Page 220
... solid and solid - solid phase changes are studied as a function of P and T. Since shear velocity is very sensitive to the presence of even a small amount of melt , sudden decreases in ẞ ( r ) can be related to the solidus within the ...
... solid and solid - solid phase changes are studied as a function of P and T. Since shear velocity is very sensitive to the presence of even a small amount of melt , sudden decreases in ẞ ( r ) can be related to the solidus within the ...
Page 226
... Solid , high - Q , self compression . f ) Phase change , possible increase in Fe / Mg , breaking down to FeO , MgO , SiO , and Al¿0 , 2. g ) Solid , high - Q , possibly superadiabatic or decreasing Fe / Mg , small lateral ...
... Solid , high - Q , self compression . f ) Phase change , possible increase in Fe / Mg , breaking down to FeO , MgO , SiO , and Al¿0 , 2. g ) Solid , high - Q , possibly superadiabatic or decreasing Fe / Mg , small lateral ...
Contents
The geodynamo | 1 |
Which solution is best | 7 |
R O VICENTE Influence of the core on the nutations | 15 |
Copyright | |
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A. E. RINGWOOD adiabatic anharmonic theory approximation axis of rotation BIRCH boundary conditions calculated chemical constant convection core-mantle boundary D. L. ANDERSON density distribution depth determined dunite dynamo action Earth models Earth Planet Earth's core eclogite elastic elastic moduli energy equation estimate experimental finite flow fluid forces fourth-order function g/cm³ Geophys geophysical Grüneisen harmonic hence high-pressure homogeneous Hugoniot indicated inertia interior JEFFREYS Journ K. E. BULLEN kbar KNOPOFF laboratory lattice layer linear Lorentz force lower mantle magnetic field magnitude material moment of inertia motion nutation observations obtained olivine oxides parameters phase changes Phys physical precession pressure problem properties pyroxene region RINGWOOD S-waves seismic velocities seismology shear shock silicates solid solution spheroid spinel stishovite strain structure surface theoretical thermal thermal equation tion toroidal upper mantle variation vector viscosity wave-guides waves