The Role of CO2 in Aqueous Alteration of Ultra-Mafic Rocks and the Formation of Mg-, Fe-rich Aqueous Solutions on Early Mars

Details The Role of CO2 in Aqueous Alteration of Ultra-Mafic Rocks and the Formation of Mg-, Fe-rich Aqueous Solutions on Early Mars The Role of CO2 in Aqueous Alteration of Ultra-Mafic Rocks and the Formation of Mg-, Fe-rich Aqueous Solutions on Early Mars

Mar 2006

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2006lpi....37.1440n&link_type=abstract

37th Annual Lunar and Planetary Science Conference, March 13-17, 2006, League City, Texas, abstract no.1440

Physics

Scientific paper

We use data from thermodynamic modeling and studies of martian
meteorites to show that high partial pressures of CO2 were likely
present during the formation of the Mg-, Fe-rich fluids that
precipitated secondary minerals on early Mars.

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