Palagonitic (Not Andesitic) Mars: Evidence from Thermal Emission and VNIR Spectra of Palgonitic Alteration Rinds on Basaltic Rock

Physics

Scientific paper

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Scientific paper

VNIR and TES specra of palagonitic alteration rinds developed on
basaltic rocks are spectral endmembers that provide a consistent
explanation of both VNIR and TES spectra of martian dark regions.

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