The moment of inertia factor of Mars - Implications for geochemical models of the Martian interior

Details The moment of inertia factor of Mars - Implications for geochemical models of the Martian interior The moment of inertia factor of Mars - Implications for geochemical models of the Martian interior

Mar 1997

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1997lpi....28..105b&link_type=abstract

Conference Paper, 28th Annual Lunar and Planetary Science Conference, p. 105.

Mathematics

Planetary Mantles, Moments Of Inertia, Geochemistry, Planetary Cores, Iron, Planetary Composition, Mars Environment, Mathematical Models, Planetary Crusts

Scientific paper

Most models for the composition of the Martian mantle and core are dependent on knowledge of the moment of inertia factor of the planet. A lower inertia value implies a lower abundance of Fe in the Martian mantle and less S in the core, or a thicker crust. Attention is presently given to the Dreibus and Wanke (1985) geochemical model, whose mantle and core composition are derived independently of assumptions about the moment of inertia factor.

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