Other
Scientific paper
Dec 2008
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2008agufm.p53b1443m&link_type=abstract
American Geophysical Union, Fall Meeting 2008, abstract #P53B-1443
Other
5220 Hydrothermal Systems And Weathering On Other Planets, 5419 Hydrology And Fluvial Processes, 5420 Impact Phenomena, Cratering (6022, 8136), 5470 Surface Materials And Properties, 6225 Mars
Scientific paper
Phyllosilicates on Mars have been identified few years ago by the OMEGA instrument on the ESA Mars Express mission. Confirmation of the detection came recently from the CRISM spectrometer, on board the NASA's Mars Reconnaissance Orbiter. These minerals formed on Mars in the Noachian period, when moderate pH and large amount of available water occurred. Emissivity spectra of several terrestrial phyllosilicates have been measured in the Planetary Emissivity Laboratory (PEL) at DLR in Berlin, to build a spectral library of analogue materials. This dataset can be very useful for the interpretation of OMEGA and CRISM data in the 3 to 5 micron spectral region. On the other hand, such spectral library is essential for the analysis of data from the PFS on Mars Express and TES on NASA Mars Global Surveyor missions.
D'Amore Mario
Helbert Jérôme
Maturilli Alessandro
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