“…During the last twenty years high-resolution (spatial) multispectral imaging systems for photogeologic surface mapping and multi-hyperspectral sensors for thematic mapping have been developed to operate together for planetologic applications on ESA's deep space missions. Planetary spectrometers which were successfully developed, applied and operated on different European planetary projects can be divides into three groups: imaging spectrometers for the 0.25 to 5 µm range 34,35,36,37 , imaging spectrometers in the 7-14 µm region 6,8,9,53 , and interferometers 4,5,41,42,[54][55][56] . Covering the wavelength range from the UV/VIS up to the mid-infrared region, these hyperspectral systems use the reflected sunlight or the thermal emission from the different objects.…”