Origin of the martian dichotomy and Tharsis from a giant impact causing massive magmatism

Details Origin of the martian dichotomy and Tharsis from a giant impact causing massive magmatism Origin of the martian dichotomy and Tharsis from a giant impact causing massive magmatism

Sep 2011

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2011icar..215..346g&link_type=abstract

Icarus, Volume 215, Issue 1, p. 346-357.

Physics

1

Scientific paper

Dichotomous crust forms from early hemispherical magma ocean.
Tharsis-like magmatic province is formed. Volcanism is
sustained by low degree convection.

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