Инд. авторы:	Yelisseyev A.P., Khrenov A.V., Afanasiev V.P.
Заглавие:	Photoluminescence spectra of impact diamonds formed by solid-state graphite-to-diamond transition
Библ. ссылка:	Yelisseyev A.P., Khrenov A.V., Afanasiev V.P. Photoluminescence spectra of impact diamonds formed by solid-state graphite-to-diamond transition // Journal of the Optical Society of America B: Optical Physics. - 2016. - Vol.33. - Iss. 3. - P.B43-B48. - ISSN 0740-3224. - EISSN 1520-8540.
Внешние системы:	DOI: 10.1364/JOSAB.33.000B43; РИНЦ: 27145330; SCOPUS: 2-s2.0-84962053264; WoS: 000371783800006;
Реферат:	eng: Concentrations of impurities in impact diamonds (IDs) from the Popigai meteorite crater reach hundreds of parts per million and are orders of magnitude greater than those in synthetic high-pressure high-temperature diamonds. IDs belong to six groups according to photoluminescence (PL) spectra. Diamonds of groups 1 and 2, consisting of cubic and hexagonal polytypes and sometimes graphite, show PL in broad 570-620 nm bands with unusual zero-phonon lines in the near-IR range, as well as very broad Raman lines. PL spectra of other groups are dominated by signals fromnitrogen-vacancy complexes well known for kimberlite diamonds: some of them are related to radiation damage products. Variations in PL spectra are related to considerable difference in grain sizes: broadband shift to longer wavelengths and narrower lines correspond to coarser grain sizes. (C) 2016 Optical Society of America
Ключевые слова:	CRATER; CARBON; LONSDALEITE; TEMPERATURE; LUMINESCENCE; HIGH-PRESSURE; POLYCRYSTALLINE DIAMOND; NITROGEN; RAMAN;
Издано:	2016
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