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

Jean‐Pierre Bibring(Brown University), Yves Langevin(Brown University), A. Gendrin(Brown University), Brigitte Gondet(Brown University), F. Poulet(Brown University), Michel Berthé(Brown University), A. Soufflot(Brown University), Ray Arvidson(Washington University in St. Louis), N. Mangold(Brown University), J. Mustard(Brown University), P. Drossart(Brown University), the OMEGA team
Science
February 17, 2005
Cited by 954

Abstract

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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