Mars Surface Diversity as Revealed by the OMEGA/Mars Express Observations

@article{Bibring2005MarsSD,
  title={Mars Surface Diversity as Revealed by the OMEGA/Mars Express Observations},
  author={J. P. Bibring and Yves Langevin and Aline Gendrin and B. Gondet and François Poulet and Michel Berthé and Alain Soufflot and Raymond E. Arvidson and Nicolas Mangold and John F. Mustard and Pierre Drossart},
  journal={Science},
  year={2005},
  volume={307},
  pages={1576 - 1581}
}
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… 

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...

Summer Evolution of the North Polar Cap of Mars as Observed by OMEGA/Mars Express

The Observatoire pour la Mine, l'Eau, les Glaces, et l'Activite (OMEGA) visible-infrared imaging spectrometer extensively observed regions of Mars with latitudes above 70°N in late 2004 and the extent of water ice at the surface and the size of ice grains were monitored as a function of time.

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The observations of the northern circumpolar regions of Mars reveal that water alteration played a major role in the formation of the constituting minerals of northerncircumpolar terrains.

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Hyperspectral image data covering eastern Terra Meridiani indicate the ubiquitous presence of molecular water in etched terrain materials that disconformably overlie heavily cratered terrains and underlie the hematite-bearing plains explored by the Opportunity rover.

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