The Clementine Mission to the Moon: Scientific Overview

@article{Nozette1994TheCM,
  title={The Clementine Mission to the Moon: Scientific Overview},
  author={Stewart David Nozette and Pete L. Rustan and Luke Pleasance and Joseph F. Kordas and Isabella T. Lewis and H S Park and Robert E. Priest and Deirdre Horan and Paul A. Regeon and Christopher L. Lichtenberg and Eugene Merle Shoemaker and Eric M. Eliason and Alfred S. McEwen and Mark S. Robinson and Paul D. Spudis and Charles H. Acton and Bonnie J. Buratti and Thomas C. Duxbury and Daniel N. Baker and Bruce M. Jakosky and Jacques E. Blamont and Michael Corson and Joshua H. Resnick and Chris Rollins and Merton E. Davies and Paul G. Lucey and Erick R. Malaret and Mark Alan Massie and Carle M. Pieters and Robert A. Reisse and Richard A. Simpson and D. E. Smith and Todd C. Sorenson and R W Breugge and Maria T. Zuber},
  journal={Science},
  year={1994},
  volume={266},
  pages={1835 - 1839}
}
In the course of 71 days in lunar orbit, from 19 February to 3 May 1994, the Clementine spacecraft acquired just under two million digital images of the moon at visible and infrared wavelengths. These data are enabling the global mapping of the rock types of the lunar crust and the first detailed investigation of the geology of the lunar polar regions and the lunar far side. In addition, laser-ranging measurements provided the first view of the global topographic figure of the moon. The… 
The Shape and Internal Structure of the Moon from the Clementine Mission
TLDR
Global topographic and gravitational field models derived from data collected by the Clementine spacecraft reveal a new picture of the shape and internal structure of the moon, indicating that the structure and thermal history of the Moon are more complex than was previously believed.
Advances in lunar science from the Clementine mission: A decadal perspective
The Clementine spacecraft orbited the Moon and acquired science data for 10 weeks in the Spring of 1994. During this time it collected global 11-band multispectral images and near global altimetry.
A New View of the Moon in Light of Data from Clementine and Prospector Missions
Results from the 1994 Clementine and 1998–99 Lunar Prospector orbital missions are forcing a reevaluation of existing models of the origin and evolution of the Moon. Data on global topography and
The South Pole Region of the Moon as Seen by Clementine
TLDR
The Clementine mission has provided the first comprehensive set of high-resolution images of the south pole region of the moon and the Schr�dinger Basin, one of the two youngest, least modified, great multiring impact basins on the moon.
Topography of the Moon from the Clementine
Range measurements from the lidar instrument carried aboard the Clementine spacecraft have been used to produce an accurate global topographic model of the Moon. This paper discusses the function of
Mapping of the Moon by Clementine
Topography of the Moon from the Clementine lidar
Range measurements from the lidar instrument carried aboard the Clementine spacecraft have been used to produce an accurate global topographic model of the Moon. This paper discusses the function of
New lunar gravity and topography data from the Clementine Mission provide a global
New lunar gravity and topography data from the Clementine Mission provide a global Bouguer anomaly map corrected for the gravitational attraction of mare fill in mascon basins. Most of the gravity
New Views of Lunar Geoscience: An Introduction and Overview
Beyond the Earth, the Moon is the only planetary body for which we have samples from known locations. The analysis of these samples gives us “ground-truth” for numerous remote sensing studies of the
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References

SHOWING 1-10 OF 21 REFERENCES
The Shape and Internal Structure of the Moon from the Clementine Mission
TLDR
Global topographic and gravitational field models derived from data collected by the Clementine spacecraft reveal a new picture of the shape and internal structure of the moon, indicating that the structure and thermal history of the Moon are more complex than was previously believed.
The South Pole Region of the Moon as Seen by Clementine
TLDR
The Clementine mission has provided the first comprehensive set of high-resolution images of the south pole region of the moon and the Schr�dinger Basin, one of the two youngest, least modified, great multiring impact basins on the moon.
Preliminary results of the Apollo 17 infrared scanning radiometer
The thermal emission of the lunar surface has been mapped by an infrared scanner from lunar orbit. Samples from approximately 2.5 × 105 scans reveal the full range of lunar temperatures from 80 K to
Topographic-Compositional Units on the Moon and the Early Evolution of the Lunar Crust
TLDR
The lack of fill of the South Pole—Aitken Basin by mare basalts suggests poor production efficiency of mare basalt in the mantle of this area of the moon.
The sunlit lunar surface
Certain studies were made of the lunar surface based on measurements at visible and far infrared wavelengths obtained from a scan over the full Moon. The large number of data points available made it
Clementine Observations of the Aristarchus Region of the Moon
TLDR
Multispectral and topographic data acquired by the Clementine spacecraft provide information on the composition and geologic history of the Aristarchus region of the moon, revealing olivine-rich materials and two kilometer-sized outcrops of anorthosite in the central peaks.
Evaluation of infrared emission spectroscopy for mapping the moon's surface composition from lunar orbit
Infrared thermal emission spectroscopy is evaluated for its possible application to compositional mapping of the Moon's surface from lunar orbit. Principles of the mid-IR (∼4–25 μm) technique,
Ancient Multiring Basins on the Moon Revealed by Clementine Laser Altimetry
TLDR
Analysis of laser altimetry data from Clementine has confirmed and extended knowledge of nearly obliterated multiring basins on the moon, and several additional depressions seen in the data may represent previously unmapped ancient impact basins.
A Sharper View of Impact Craters from Clementine Data
TLDR
The ultraviolet-visible camera on the Clementine spacecraft obtained high-spatial resolution images of the moon in five spectral channels that show a scale of lithologic diversity that varies with crater size and target stratigraphy.
Ice in the lunar polar regions
The idea that ice and other trapped volatiles exist in permanently shadowed regions near the lunar poles was proposed by Watson, Murray, and Brown [1961]. It is reexamined in the present paper, in
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