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Clementine spacecraft

Distribution of iron on the lunar surface, as measured by the Clementine spacecraft, compared with the average iron contents (arrows) of Apollo highlands crustal rocks and lunar highlands meteorites. The meteorites, which presumably come from the nearside and farside, more closely match the global iron peak. The compositional ranges for various lunar rock types are shown as horizontal bars. [Pg.453]

Comparison of titanium contents of lunar mare basalts, as measured from neutrons by the Lunar Prospector gamma-ray spectrometer and from reflectance spectra by the Clementine spacecraft. After Prettyman et al. (2006). [Pg.456]


See other pages where Clementine spacecraft is mentioned: [Pg.34]    [Pg.68]    [Pg.34]    [Pg.68]    [Pg.15]   
See also in sourсe #XX -- [ Pg.15 , Pg.448 , Pg.455 ]




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Clementine

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