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

被引:764
作者
Bibring, JP
Langevin, Y
Gendrin, A
Gondet, B
Poulet, F
Berthé, M
Soufflot, A
Arvidson, R
Mangold, N
Mustard, J
Drossart, P
机构
[1] Inst Astrophys Spatiale, F-91405 Orsay, France
[2] Washington Univ, St Louis, MO 63130 USA
[3] IDES, F-91405 Orsay, France
[4] Brown Univ, Providence, RI 02912 USA
[5] Observ Paris, LESIA, F-92195 Meudon, France
关键词
D O I
10.1126/science.1108806
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
The Observatoire pour [a Mineralogie, l'Eau, les Glaces, et I'Activite (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 nocarbonates, 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.
引用
收藏
页码:1576 / 1581
页数:6
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