HAL (France)
open access
Improved Understanding of Lunar Surface Hydration Signatures through Comparison of Thermally Corrected Spectra from the Moon Mineralogy Mapper (M 3 )
Abstract An accurate thermal correction applied to Moon Mineralogy Mapper (M 3 ) visible/near-infrared (VNIR) spectroscopy data is necessary for proper interpretation of lunar surface hydration (i.e., OH − /H 2 O) signatures. We compare thermal correction techniques applied to both global and target
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