7.02 Physics of Mantle Convection
choice for the function F(r), at least for mantle dynamicists, is the Murnaghan EoS (Murnaghan, 1951) at constant T that allows us to write an EoS for solids of ...
Stagnant-lid convection: comparison of viscosity laws and uniform ...A large range of parameters is covered in this study and results that are obtained here for Earth's mantle are actually also relevant for icy. Fluid dynamics of planetary differentiationThe ranges given here take into account the pressure and temperature ranges that are representative of the Earth's mantle and magma oceans, and ... Analytical solutions for mantle flow in cylindrical and spherical shellsComputational models of mantle convection must accurately represent curved boundaries and the associated boundary conditions of a 3-D spherical ...
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