Artigo Acesso aberto Revisado por pares

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

2005; American Association for the Advancement of Science; Volume: 307; Issue: 5715 Linguagem: Inglês

10.1126/science.1108806

ISSN

1095-9203

Autores

Jean‐Pierre Bibring, Yves Langevin, A. Gendrin, Brigitte Gondet, F. Poulet, Michel Berthé, A. Soufflot, Ray Arvidson, N. Mangold, J. Mustard, P. Drossart,

Tópico(s)

Paleontology and Stratigraphy of Fossils

Resumo

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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