Geochemical Models of Low-Temperature Alteration of Martian Rocks

Details Geochemical Models of Low-Temperature Alteration of Martian Rocks Geochemical Models of Low-Temperature Alteration of Martian Rocks

Mar 1999

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1999lpi....30.1268w&link_type=abstract

30th Annual Lunar and Planetary Science Conference, March 15-29, 1999, Houston, TX, abstract no. 1268

Physics

4

Scientific paper

Alteration of martian basalt, T < 150oC, at high high rock/water will
yield: clay + carbonate + qz and near neutral pH water if CO2 = 6 Mbar;
and clay + serpentine + diopside, gas rich in H2, and alkaline water (to
pH ~12) if CO2 is not externally buffered.

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