The effects of deviation of Mars from its equilibrium state on the flattening of the core-mantle boundary

Computer Science

Scientific paper

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Scientific paper

In a static approach the calculations for the non-hydrostatic deviations in the core-mantle boundary have been performed for a trial interior structure model of Mars with a crust of 50 km thick (Fig.1). Mars departs from hydrostatic equilibrium to significant extent. It is seen if we compare the first even gravitational moments and for the Martian models in hydrostatic equilibrium state , with gravitational moments of the planet , [1].

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