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      Martian regolith in Elephant Moraine 79001 shock melts? Evidence from major element composition and sulfur speciation

      Author(s): , , ,
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      Journal: Geochimica et Cosmochimica Acta
      Publisher: Elsevier BV

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          Mars surface diversity as revealed by the OMEGA/Mars Express observations.

          Jean-Pierre Bibring, Yves Langevin, Aline Gendrin … (2005)
          The Observatoire pour la Minéralogie, l'Eau, les Glaces, et l'Activité (OMEGA) investigation, on board the European Space Agency Mars Express mission, is mapping the surface composition of Mars at a 0.3- to 5-kilometer resolution by means of visible-near-infrared hyperspectral reflectance imagery. The data acquired during the first 9 months of the mission already reveal a diverse and complex surface mineralogy, offering key insights into the evolution of Mars. OMEGA has identified and mapped mafic iron-bearing silicates of both the northern and southern crust, localized concentrations of hydrated phyllosilicates and sulfates but no carbonates, and ices and frosts with a water-ice composition of the north polar perennial cap, as for the south cap, covered by a thin carbon dioxide-ice veneer.
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            Shock metamorphism of ordinary chondrites

            Dieter Stöffler, Klaus Keil, Scott Edward R.D (1991)
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              The composition of the atmosphere at the surface of Mars

              A L Lafleur, Tobias Owen, K Biemann … (1977)
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                Author and article information

                Journal
                Title: Geochimica et Cosmochimica Acta
                Abbreviated Title: Geochimica et Cosmochimica Acta
                Publisher: Elsevier BV
                ISSN (Print): 00167037
                Publication date Created: August 2010
                Publication date (Print): August 2010
                Volume: 74
                Issue: 16
                Pages: 4829-4843
                Article
                DOI: 10.1016/j.gca.2010.04.065
                SO-VID: e2f353e9-dfdd-4490-bb34-2e55bd38e69d
                Copyright © © 2010
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                http://www.elsevier.com/tdm/userlicense/1.0/

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