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Mineralogical Magazine; April 2004; v. 68; no. 2; p. 323-333; DOI: 10.1180/0026461046820189
© Mineralogical Society of Great Britain and Ireland
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FIG. 10. Reflectance values from a given mineral surface obey a reasonably multigaussian distribution as shown here for true colour intensities from a 20x20 pixels region in bornite from Kipushi.





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