Measurements of absolute thorium abundances on the lunar surface are presen
ted using both the high- and low-altitude data taken with the Lunar Prospec
tor Gamma-Ray Spectrometer. An analysis of the uncertainties shows that the
measured uncertainties are < 0.5 mu g/g and are close to the theoretical l
imit of Poisson statistics. Currently, the overall systematic uncertainties
are likely dominated by variations in background counts. The relative syst
ematic uncertainties are thought to be no larger than 30% for the high-alti
tude data and 15% for the low-altitude data. A comparison of high- and low-
altitude data show that most regions having thorium abundances > 7 mu g/g a
re likely small area regions less than or equal to (150 km)(2). Using lunar
topographic data, we have shown that the thorium abundances in the lunar h
ighlands and portions of South Pole-Aitken (SPA) Basin are larger for lower
elevations. We have also studied a number of regions with anomalously high
thorium abundances such as the northwestern region of SPA Basin, the crate
r Arago in western Tranquillitatis, and the Compton/Belkovich region in the
northeastern highlands. The Compton/Belkovich region appears to be enriche
d with evolved rocks such as alkali anorthosite and currently represents th
e only such extended region on the Moon that has been identified. In contra
st, Tycho crater has very low thorium abundances which suggests that KREEP
was not assimilated at depth in this portion of the Moon.