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Science 29 March 1968: Vol. 159. no. 3822, pp. 1453 - 1455 DOI: 10.1126/science.159.3822.1453
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Articles
Lunar and Martian Surfaces: Petrologic Significance of Absorption Bands in the Near-Infrared
John B. Adams 1
1 Jet Propulsion Laboratory, California Institute of Technology, Pasadena 91103
A reflection minimum at 1 micron, reported for Moon and for Mars, indicates olivine or iron- and calcium-bearing clinopyroxene, or bothmajor constituents of many basaltic rocks. If the 1-micron absorption features are real, both chondritic and acidic rocks are ruled out as primary constituents of the surfaces of the bodies. The reflectance spectrum of Mars matches closely that of an oxidized basalt.
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- D. R. Waldbaum and D. R. Waldbaum (1969)
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