How Can We Reconcile Mars Thermal History with the Crustal Dichotomy, Magnetic Field, and Tharsis Volcanism?

Details How Can We Reconcile Mars Thermal History with the Crustal Dichotomy, Magnetic Field, and Tharsis Volcanism? How Can We Reconcile Mars Thermal History with the Crustal Dichotomy, Magnetic Field, and Tharsis Volcanism?

Mar 2006

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2006lpi....37.1927k&link_type=abstract

37th Annual Lunar and Planetary Science Conference, March 13-17, 2006, League City, Texas, abstract no.1927

Physics

Scientific paper

The interior heat engine is the primary driving mechanism for
planetary-scale tectonic and volcanic processes; hence it is important
to understand whether our picture of Martian thermal evolution is
consistent with these events.

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