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Abstract Raman spectra of cornetite, libethenite, pseudomalachite, reichenbachite and ludjibaite were obtained at 298 and 77 K using a Raman microprobe in combination with a thermal stage. Raman spectra of cornetite, libethenite and pseudomalachite are different, in line with differences in crystal structure and composition. Raman spectra of the three polymorphs pseudomalachite, reichenbachite and ludjibaite are similar, particularly in the stretching region, but characteristic differences in the deformation regions are observed. Differences are also observed in the phosphate deformation and stretching regions. Copyright © 2002 John Wiley & Sons, Ltd.
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Ray L. Frost
Universidade Federal de Ouro Preto
Peter A. Williams
University College of the North
Wayde N. Martens
Queensland University of Technology
Journal of Raman Spectroscopy
Queensland University of Technology
Western Sydney University
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Frost et al. (Fri,) studied this question.
synapsesocial.com/papers/6a214225a16f1d2b6a5acb97 — DOI: https://doi.org/10.1002/jrs.850