Characterization of lunar mare basalt types. II - Spectral classification of fresh mare craters

Telescopic reflectance spectra (0.3-1.1 microns) of fresh craters are presented and classified according to the spectral features observed. These spectra are the closest lunar surface analog to laboratory spectra obtained for lunar rock powders. Mineral absorption features can be identified in these crater spectra and interpreted using returned lunar samples. Spectra of craters to 2.5 microns are required for specific mineralogical determinations from remote observation. If the currently available telescopic spectra are representative, classification of lunar telescopic spectra indicates that most (more than 80%) of the lunar surface is composed of a finite number of discrete and describable geochemical units.