Инд. авторы: | Golovin A.V., Goryainov S.V., Kokh S.N., Sharygin I.S., Rashchenko S.V., Kokh K.A., Sokol E.V., Devyatiyarova A.S. |
Заглавие: | The application of Raman spectroscopy to djerfisherite identification |
Библ. ссылка: | Golovin A.V., Goryainov S.V., Kokh S.N., Sharygin I.S., Rashchenko S.V., Kokh K.A., Sokol E.V., Devyatiyarova A.S. The application of Raman spectroscopy to djerfisherite identification // Journal of Raman Spectroscopy. - 2017. - Vol.48. - Iss. 11. - P.1574-1582. - ISSN 0377-0486. - EISSN 1097-4555. |
Внешние системы: | DOI: 10.1002/jrs.5210; РИНЦ: 31075505; WoS: 000416235800027; |
Реферат: | eng: Raman spectra were acquired from the synthetic cubic K6Fe25S26Cl phase (55.3wt% Fe) and ten natural djerfisherites K-6(Fe,Cu,Ni)(25)S26Cl with various contents of Fe (from 15.5 to 22.6 atoms per formula unit (apfu)) and Ni+Cu+Co (from 1.4 to 9.0 apfu). The natural samples came from rocks of the Udachnaya, Obnazhennaya and Vtorogodnitsa kimberlite pipes and high-grade contact marbles near Kochumdek River (Siberian craton, Russia). Diagnostic features of both synthetic and natural djerfisherite Raman spectra can be summarized as follows: the presence of two strong bands at 264-273 and 321-344cm(-1) and from two to five medium/weak bands in the region from 90 to 190cm(-1). Raman spectra of Fe-rich ((Ni+Cu+Co)<2.4 apfu) djerfisherite have up to nine bands, whereas the number of Raman bands in spectra of djerfisherite with high impurity concentration ((Ni+Cu+Co)=8.7-9 apfu) reduces to four. The Raman spectra of djerfisherite enriched in impurities ((Ni+Cu+Co)=5-9 apfu) are also characterized by broadening and asymmetry of bands in comparison with Ni+Cu+Co-poor djerfisherite. Experimental Raman spectra of synthetic and natural djerfisherites show good agreement with theoretical spectra calculated using lattice-dynamical software. The group of bands in the range 90-190cm(-1) is associated with the S-Fe-S bending vibrations in FeS4 tetrahedra and FeS6 octahedra. The band group in the range of 260-350cm(-1) is due to the Fe-S stretching vibrations in both polyhedra. Copyright (c) 2017 John Wiley & Sons, Ltd.
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Ключевые слова: | mantle xenoliths; high-grade contact marbles; Raman spectroscopy; UDACHNAYA-EAST PIPE; MELT INCLUSIONS; UNALTERED KIMBERLITES; djerfisherite; ENSTATITE CHONDRITES; DIAMOND FORMATION; CRYSTAL-STRUCTURE; YAKUTIA; SIBERIA; RUSSIA; KOLA-PENINSULA; kimberlites; |
Издано: | 2017 |
Физ. характеристика: | с.1574-1582 |