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      The petrological expression of early Mars volcanism : EARLY MARS VOLCANISM

      , , ,
      Journal of Geophysical Research: Planets
      American Geophysical Union (AGU)

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          Global mineralogical and aqueous mars history derived from OMEGA/Mars Express data.

          Global mineralogical mapping of Mars by the Observatoire pour la Mineralogie, l'Eau, les Glaces et l'Activité (OMEGA) instrument on the European Space Agency's Mars Express spacecraft provides new information on Mars' geological and climatic history. Phyllosilicates formed by aqueous alteration very early in the planet's history (the "phyllocian" era) are found in the oldest terrains; sulfates were formed in a second era (the "theiikian" era) in an acidic environment. Beginning about 3.5 billion years ago, the last era (the "siderikian") is dominated by the formation of anhydrous ferric oxides in a slow superficial weathering, without liquid water playing a major role across the planet.
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            The pMELTS: A revision of MELTS for improved calculation of phase relations and major element partitioning related to partial melting of the mantle to 3 GPa

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              Algorithmic modifications extending MELTS to calculate subsolidus phase relations

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                Author and article information

                Journal
                Journal of Geophysical Research: Planets
                J. Geophys. Res. Planets
                American Geophysical Union (AGU)
                21699097
                January 2013
                January 30 2013
                : 118
                : 1
                : 59-64
                Article
                10.1029/2012JE004234
                1c1b8e11-4c21-48d3-b53c-44a05f46f8b6
                © 2013

                http://doi.wiley.com/10.1002/tdm_license_1.1

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