Thermal Evolution of Mercury in the Conductive Regime and Implications for Magnetism

Details Thermal Evolution of Mercury in the Conductive Regime and Implications for Magnetism Thermal Evolution of Mercury in the Conductive Regime and Implications for Magnetism

Mar 2002

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2002lpi....33.1998r&link_type=abstract

33rd Annual Lunar and Planetary Science Conference, March 11-15, 2002, Houston, Texas, abstract no.1998

Physics

Scientific paper

Models of thermal evolution of Mercury with realistic temperature and
pressure-dependent viscosity suggest that convection ceased early. A
conductive mantle can explain generation of a small magnetic field.

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