Viscoelastic Finite-Element Simulations of the Flexure Under the North Polar Cap of Mars

Details Viscoelastic Finite-Element Simulations of the Flexure Under the North Polar Cap of Mars Viscoelastic Finite-Element Simulations of the Flexure Under the North Polar Cap of Mars

Mar 2010

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2010lpi....41.1865d&link_type=abstract

41st Lunar and Planetary Science Conference, held March 1-5, 2010 in The Woodlands, Texas. LPI Contribution No. 1533, p.1865

Physics

1

Scientific paper

The thick lithosphere may be explained if the mantle and crust are
subchondritic and if there is a strong depletion of heat-producing
elements in the mantle, possibly a result of the formation of the
crustal dichotomy via a giant impact.

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