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Global Mineralogical and Aqueous Mars History Derived from OMEGA/Mars Express Data
DOI: 10.1126/science.1122659 Bibcode: 2006Sci...312..400B

Drossart, Pierre; Korablev, Oleg; Forget, F. +43 more

Global mineralogical mapping of Mars by the Observatoire pour la Mineralogie, l'Eau, les Glaces et l'Activité (OMEGA) instrument on the European Space Agency's Mars Express spacecraft provides new information on Mars' geological and climatic history. Phyllosilicates formed by aqueous alteration very early in the planet's history (the ``phyllocian'…

2006 Science
MEx 1327
Formation of Glaciers on Mars by Atmospheric Precipitation at High Obliquity
DOI: 10.1126/science.1120335 Bibcode: 2006Sci...311..368F

Forget, F.; Montmessin, F.; Head, J. W. +2 more

Surface conditions on Mars are currently cold and dry, with water ice unstable on the surface except near the poles. However, geologically recent glacierlike landforms have been identified in the tropics and the midlatitudes of Mars. The ice has been proposed to originate from either a subsurface reservoir or the atmosphere. We present high-resolu…

2006 Science
MEx 361
Plasma Acceleration Above Martian Magnetic Anomalies
DOI: 10.1126/science.1122071 Bibcode: 2006Sci...311..980L

Coates, A. J.; Kallio, E.; Fedorov, A. +20 more

Auroras are caused by accelerated charged particles precipitating along magnetic field lines into a planetary atmosphere, the auroral brightness being roughly proportional to the precipitating particle energy flux. The Analyzer of Space Plasma and Energetic Atoms experiment on the Mars Express spacecraft has made a detailed study of acceleration p…

2006 Science
MEx 104