Mantle Plumes and Long-lived Volcanism on Mars as a Result of Compositional Layering

Details Mantle Plumes and Long-lived Volcanism on Mars as a Result of Compositional Layering Mantle Plumes and Long-lived Volcanism on Mars as a Result of Compositional Layering

Mar 2007

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2007lpi....38.2133z&link_type=abstract

38th Lunar and Planetary Science Conference, (Lunar and Planetary Science XXXVIII), held March 12-16, 2007 in League City, Texas

Physics

Scientific paper

To address the influence of a deep, dense mantle layer on the thermal
evolution of the martian interior, we use a series of 1D numerical
convection simulations. Mantle layering is found to increase both the
amount and duration of melting.

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