Global maps of thermal and fast neutron fluxes from the moon suggest t
hree end-member compositional units. A high thermal and Low fast neutr
on flux unit correlates with the Lunar highlands and is consistent wit
h feldspathic rocks. The South Pole-Aitken basin and a strip that surr
ounds the nearside maria have intermediate thermal and fast neutron fl
ux Levels, consistent with more mafic rocks. There appears to be a smo
oth transition between the most mafic and feldspathic compositions, wh
ich correspond to Low and high surface altitudes, respectively. The ma
ria show Low thermal and high fast neutron fluxes, consistent with bas
altic rocks.