Fig. 36. Reflectance Spectra of Two Carbonaceous Chondritic Meteorites (Murchison and Orguiel).

Orgueil data from Feierberg (unpublished), Murchison data from Lebofsky et al (1982). The absolute reflectance of the Orgueil sample was not obtained, and is here assumed to equal that of Murchison at 2 microns. The Orgueil spectrum, obtained only longward of 1.8 microns, has been extended down to 0.7 microns using the result from Johnson et al (1973) that the spectrum is flat in this range.
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