Giant Impacts and Thermochemical Martian Mantle Convection: Implications for Tharsis

Details Giant Impacts and Thermochemical Martian Mantle Convection: Implications for Tharsis Giant Impacts and Thermochemical Martian Mantle Convection: Implications for Tharsis

Mar 2003

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2003lpi....34.1442r&link_type=abstract

34th Annual Lunar and Planetary Science Conference, March 17-21, 2003, League City, Texas, abstract no.1442

Computer Science

Scientific paper

The initial thermal and compositional state of Mars was likely
heterogeneous as a result of giant impacts. Finite element simulations
suggest that impact-induced compositional differentiation may play an
important role in Martian evolution.

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