The Crustal Dichotomy and Edge Driven Convection: A Mechanism for Tharsis Rise Volcanism?

Details The Crustal Dichotomy and Edge Driven Convection: A Mechanism for Tharsis Rise Volcanism? The Crustal Dichotomy and Edge Driven Convection: A Mechanism for Tharsis Rise Volcanism?

Mar 2005

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2005lpi....36.1960k&link_type=abstract

36th Annual Lunar and Planetary Science Conference, March 14-18, 2005, in League City, Texas, abstract no.1960

Physics

2

Scientific paper

This work uses numerical modeling and analysis of the Martian areoid to
assess the conditions underwhich edge driven convection could form
Tharsis rise.

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