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Single-crystal structure and Raman spectroscopy of synthetic titanite analog CaAlSiO<inf>4</inf>F

dc.contributor.authorTroitzsch, Ulrike
dc.contributor.authorKruger, Hannes
dc.contributor.authorTobbens, Daniel M.
dc.contributor.authorTropper, Peter
dc.contributor.authorHaefeker, Udo
dc.contributor.authorKahlenberg, Volker
dc.contributor.authorFuchs, Martin R.
dc.contributor.authorOlieric, Vincent
dc.date.accessioned2016-02-24T22:40:33Z
dc.date.issued2015
dc.date.updated2016-02-24T08:06:29Z
dc.description.abstractSynthetic CaAlSiO<inf>4</inf>F, the Al-F analog of titanite, has been investigated using single-crystal synchrotron diffraction experiments at Beamline X06DA (Swiss Light Source, Paul Scherrer Institute, Villigen, Switzerland) and Raman spectroscopy. The presented structural model with 40 parameters was refined against 506 unique reflections to a final R<inf>obs</inf> of 0.026 (space group A2/a, a = 6.9120(11), b = 8.5010(10), c = 6.435(2) Å, β = 114.670(11)°, and Z = 4) and exhibits less distorted coordination polyhedra than earlier models from powder data. Vibrational spectra were calculated in harmonic approximation at the Γ point from fully relaxed energy optimisations of the crystal structure, using 3D-periodic density functional theory with Gaussian basis sets and the software CRYSTAL06. The lattice parameters of the fully relaxed structure were in good agreement with the experimental values, with the calculated values 0.8 ± 0.4 % too large; the monoclinic angle was calculated 0.4° too large. The agreement of the calculated Raman frequencies with the observed ones was very good, with standard deviation ±3 cm−1 and maximum deviations of ±7 cm−1. Furthermore, a detailed discussion of the atomic displacements associated with each Raman mode is given.
dc.identifier.issn0930-0708
dc.identifier.urihttp://hdl.handle.net/1885/98360
dc.publisherSpringer
dc.sourceMineralogy and Petrology
dc.titleSingle-crystal structure and Raman spectroscopy of synthetic titanite analog CaAlSiO<inf>4</inf>F
dc.typeJournal article
local.bibliographicCitation.issue5
local.bibliographicCitation.lastpage641
local.bibliographicCitation.startpage631
local.contributor.affiliationTroitzsch, Ulrike, College of Physical and Mathematical Sciences, ANU
local.contributor.affiliationKruger, Hannes, University of Innsbruck
local.contributor.affiliationTobbens, Daniel M., Helmholtz-Zentrum Berlin fur Materialien und Energie GmbH
local.contributor.affiliationTropper, Peter, University of Innsbruk
local.contributor.affiliationHaefeker, Udo, University of Innsbruck
local.contributor.affiliationKahlenberg, Volker, University of Innsbruck
local.contributor.affiliationFuchs, Martin R. , Paul Scherrer Institute
local.contributor.affiliationOlieric, Vincent, Paul Scherrer Institute
local.contributor.authoruidTroitzsch, Ulrike, u4033864
local.description.embargo2037-12-31
local.description.notesImported from ARIES
local.identifier.absfor030200 - INORGANIC CHEMISTRY
local.identifier.absfor040300 - GEOLOGY
local.identifier.ariespublicationa383154xPUB2608
local.identifier.citationvolume109
local.identifier.doi10.1007/s00710-015-0393-3
local.identifier.scopusID2-s2.0-84934784241
local.type.statusPublished Version

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