New Insights into the Nature of Mineralogic Alteration on Mars from Orbiter, Rover, and Laboratory Data

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Scientific paper

TES spectra now appear to support the identification in some places of
phyllosilicates observed by OMEGA/CRISM. Enigmatically, spectra from
Mini-TES in Gusev crater show no such phases on rocks that clearly are
altered. Amorphous phases are implicated.

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