Please use this identifier to cite or link to this item: http://elar.urfu.ru/handle/10995/89970
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dc.contributor.authorAlifirova, T.en
dc.contributor.authorRezvukhin, D.en
dc.contributor.authorNikolenko, E.en
dc.contributor.authorPokhilenko, L.en
dc.contributor.authorZelenovskiy, P.en
dc.contributor.authorSharygin, I.en
dc.contributor.authorKorsakov, A.en
dc.contributor.authorShur, V.en
dc.contributor.authorШур, В. Я.ru
dc.date.accessioned2020-09-29T09:45:28Z-
dc.date.available2020-09-29T09:45:28Z-
dc.date.issued2020-
dc.identifier.citationMicro-Raman study of crichtonite group minerals enclosed into mantle garnet / T. Alifirova, D. Rezvukhin, E. Nikolenko, L. Pokhilenko, et al. . — DOI 10.1002/jrs.5979 // Journal of Raman Spectroscopy. — 2020. — Vol. 9. — Iss. 51. — P. 1493-1512.en
dc.identifier.issn0377-0486-
dc.identifier.otherhttps://onlinelibrary.wiley.com/doi/pdfdirect/10.1002/jrs.5979pdf
dc.identifier.other1good_DOI
dc.identifier.other0f2a1038-71f9-4517-9a1f-f6e2e796567epure_uuid
dc.identifier.otherhttp://www.scopus.com/inward/record.url?partnerID=8YFLogxK&scp=85091041484m
dc.identifier.urihttp://elar.urfu.ru/handle/10995/89970-
dc.description.abstractWe report the first comprehensive micro-Raman study of crichtonite group minerals (CGM) as inclusions in pyropic garnet grains from peridotite and pyroxenite mantle xenoliths of the Yakutian kimberlites as well as in garnet xenocrysts from the Aldan shield lamprophyres (Russia). The CGM form (i) morphologically oriented needles, lamellae, and short prisms and (ii) optically unoriented subhedral to euhedral grains, either single or intergrown with other minerals. We considered common mantle-derived CGM species (like loveringite, lindsleyite, and their analogues), with Ca, Ba, or Sr dominating in the dodecahedral A site and Zr or Fe in the octahedral B site. The Raman bands at the region of 600–830 cm−1 are indicative of CGM and their crystal-chemical distinction, although the intensity and shape of the bands appear to be dependent on laser beam power and wavelength. The factor-group analysis based on the loveringite crystal structure showed the octahedral and tetrahedral cation groups with 18f and 6c Wyckoff positions, namely, dominantly TiO6 and to a lower extent CrO6, MgO4, and FeO4 groups, to be the major contributors to the Raman spectral features. The ionic groups with dodecahedral (M0) and octahedral (M1) coordination are inactive for Raman scattering while active in infrared absorption. A number of observed Raman modes in the CGM spectra are several times lower than that predicted by the factor group analysis. The noticed broadening of modes in the CGM Raman spectra may result from a combining of bands at the narrow frequency shift regions. Solid solution behavior, luminescence, and partial metamictization of the CGM may exert additional influence on the Raman band shape. The Raman spectral features showed CGM to be accurately identified and distinguished from other Ti-, Fe-, Cr-, and Zr-containing oxides (e.g., ilmenite or those of spinel and magnetoplumbite groups) occurring as accessory mantle minerals. © 2020 The Authors. Journal of Raman Spectroscopy published by John Wiley & Sons Ltden
dc.description.sponsorshipRussian Science Foundation, RSF: 18‐77‐10062en
dc.description.sponsorshipCouncil on grants of the President of the Russian Federationen
dc.description.sponsorshipThis study was supported by the Russian Science Foundation (Grant 18‐77‐10062). The equipment of the Ural Center for Shared Use «Modern Nanotechnology», Ural Federal University, and the Analytical Center for Multi‐elemental and Isotope Research, IGM, was used. Sampling was supported by the Russian Federation state assignment project of IGM. We are grateful to Nikolai V. Sobolev for Samples O‐173, O‐39, and O‐264. Vladimir N. Korolyuk, Elena N. Nigmatulina (IGM), and Allan Patchen (UT) are highly appreciated for the help with EMP analyses. We express our sincere thanks to F. Nestola and an anonymous reviewer for their thorough reviews and helpful suggestions, and to C. Marshall for regardful editorial handling of the manuscript on every stage of its revision.en
dc.format.mimetypeapplication/pdfen
dc.language.isoenen
dc.publisherJohn Wiley and Sons Ltden
dc.relationinfo:eu-repo/grantAgreement/RSF//18-77-10062en
dc.rightsinfo:eu-repo/semantics/openAccessen
dc.rightscc-byother
dc.sourceJournal of Raman Spectroscopyen
dc.subjectCRICHTONITE GROUP MINERALSen
dc.subjectMANTLE XENOLITHSen
dc.subjectORIENTED INCLUSIONSen
dc.subjectPYROPEen
dc.subjectRAMAN SPECTROSCOPYen
dc.titleMicro-Raman study of crichtonite group minerals enclosed into mantle garneten
dc.typeArticleen
dc.typeinfo:eu-repo/semantics/articleen
dc.typeinfo:eu-repo/semantics/publishedVersionen
dc.identifier.doi10.1002/jrs.5979-
dc.identifier.scopus85091041484-
local.affiliationSobolev Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences, Novosibirsk, Russian Federationen
local.affiliationDepartment of Lithospheric Research, University of Vienna, Vienna, Austriaen
local.affiliationGeo-Scientific Research Enterprise ALROSA (PJSC), Mirny, Russian Federationen
local.affiliationInstitute of Natural Sciences and Mathematics, Ural Federal University, Ekaterinburg, Russian Federationen
local.affiliationInstitute of the Earth's Crust, Siberian Branch, Russian Academy of Sciences, Irkutsk, Russian Federationen
local.contributor.employeeAlifirova, T., Sobolev Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences, Novosibirsk, Russian Federation, Department of Lithospheric Research, University of Vienna, Vienna, Austriaru
local.contributor.employeeRezvukhin, D., Sobolev Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences, Novosibirsk, Russian Federationru
local.contributor.employeeNikolenko, E., Sobolev Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences, Novosibirsk, Russian Federation, Geo-Scientific Research Enterprise ALROSA (PJSC), Mirny, Russian Federationru
local.contributor.employeePokhilenko, L., Sobolev Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences, Novosibirsk, Russian Federationru
local.contributor.employeeZelenovskiy, P., Institute of Natural Sciences and Mathematics, Ural Federal University, Ekaterinburg, Russian Federationru
local.contributor.employeeSharygin, I., Sobolev Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences, Novosibirsk, Russian Federation, Institute of the Earth's Crust, Siberian Branch, Russian Academy of Sciences, Irkutsk, Russian Federationru
local.contributor.employeeKorsakov, A., Sobolev Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences, Novosibirsk, Russian Federationru
local.contributor.employeeShur, V., Institute of Natural Sciences and Mathematics, Ural Federal University, Ekaterinburg, Russian Federationru
local.description.firstpage1493-
local.description.lastpage1512-
local.issue51-
local.volume9-
dc.identifier.wos000569081500001-
local.identifier.pure13913344-
local.identifier.eid2-s2.0-85091041484-
local.fund.rsf18-77-10062-
local.identifier.wosWOS:000569081500001-
Appears in Collections:Научные публикации ученых УрФУ, проиндексированные в SCOPUS и WoS CC

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