Integration of the Clementine UV-VIS spectral reflectance data and the Lunar Prospector gamma-ray spectrometer data: A global-scale multielement analysis of the lunar surface using iron, titanium, and thorium abundances

Details Integration of the Clementine UV-VIS spectral reflectance data and the Lunar Prospector gamma-ray spectrometer data: A global-scale multielement analysis of the lunar surface using iron, titanium, and thorium abundances Integration of the Clementine UV-VIS spectral reflectance data and the Lunar Prospector gamma-ray spectrometer data: A global-scale multielement analysis of the lunar surface using iron, titanium, and thorium abundances

Dec 2002

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2002jgre..107.5132c&link_type=abstract

Journal of Geophysical Research (Planets), Volume 107, Issue E12, pp. 15-1, CiteID 5132, DOI 10.1029/2000JE001419

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10

Planetology: Solar System Objects: Moon (1221), Planetology: Comets And Small Bodies: Remote Sensing, Planetology: Fluid Planets: Surfaces, Planetology: Comets And Small Bodies: Radiation And Spectra, Planetology: Fluid Planets: Composition

Scientific paper

We present a statistical analysis, based on a systematic clustering method, of a data set integrating the global abundances maps of iron, titanium, and thorium derived from Clementine and Lunar Prospector. Homogeneous geological units are compositionally characterized and spatially defined in relation to the major rock types sampled on the Moon. With the lowest abundances in Fe, Ti, and Th found on the Moon, the lunar highlands terrains are quite homogeneous with two major large feldspathic units, one being slightly more mafic than the other. Two distinct regions with unique compositions are unambiguously identified: the Procellarum KREEP Terrane (PKT) and the South Pole-Aitken (SPA). The PKT, which includes all the units with Th abundances higher than 3.5 ppm (KREEP-rich materials), is delimited by an almost continuous ring-like unit. In particular, it includes the western nearside maria, except for Mare Humorum. Within the PKT a Th-rich unit, corresponding to the highest Th concentrations found on the Moon, may represent KREEP volcanic deposits excavated from relatively shallow depth. With concentrations in Fe, Ti, and Th enhanced relative to the surrounding highlands, the South Pole-Aitken basin floor represents a large mafic anomaly on the farside, suggesting wide deposits of lower crust and possible mantle materials. However, due to indirect residual latitude effects in the Clementine spectral reflectance measurements, iron abundances might have been overestimated in SPA, thus implying that crustal materials, rather than mantle materials, might represent the dominant contributor to the mafic component exposed on the basin floor.

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