The thermo-chemical evolution of Mars with a strongly stratified mantle
Abstract. The Martian mantle probably experienced an early global magma ocean stage. The crystallization and the fractionation and overturn of such a magma ...
7.02 Physics of Mantle Convectionchoice 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 ...
Autres Cours:
