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1 Institute of Geochemistry, Mineralogy and Ore Formation, National Academy of Sciences of Ukraine, Palladin Ave. 34, 03680 Kyiv-142, Ukraine
2 Institut für Angewandte Geowissenschaften I, Technische Universität, Ernst-Reuter-Platz 1, D-10587 Berlin, Germany
* Corresponding author, e-mail: taran{at}mineral.freenet.kiev.ua
A distinctive feature of Ukrainian deep-violet diamond microcrystals is a broad absorption band centered at about 560 nm (17850 cm1 or 2.21 eV). In the Ukrainian samples, the intensity of this band is almost two orders of magnitude greater than in a light-rose diamond from Yakutia. Previously (Taran et al., 1998), the band was attributed to the N-V center because the absorption spectrum of the negative N-V center in irradiated and annealed type Ib diamonds is known to have an absorption band with a maximum at a similar wavelength. However, this assignment is not confirmed by vibrational spectroscopy and low temperature optical absorption spectroscopy in all crystals studied. In addition, at
77 K the band 17850 cm1 displays no fine structure that unambiguously evidences that it can not be the band at
2.2 eV, commonly attributed to the N-V center.
Key-words: diamond, electronic and vibrational spectroscopy.
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M. N. TARAN, V. M. KVASNYTSYA, K. LANGER, and K. O. ILCHENKO Infrared spectroscopy study of nitrogen centers in microdiamonds from Ukrainian Neogene placers European Journal of Mineralogy, February 1, 2006; 18(1): 71 - 81. [Abstract] [Full Text] [PDF] |
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