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dc.contributor.authorTriebold, Silke
dc.contributor.authorLuvizotto, George Luiz
dc.contributor.authorTolosana Delgado, Raimon
dc.contributor.authorZack, Thomas
dc.contributor.authorvon Eynatten, Hilmar
dc.date.accessioned2011-04-07T17:06:28Z
dc.date.available2011-04-07T17:06:28Z
dc.date.created2010-07-13
dc.date.issued2010-07-13
dc.identifier.citationTriebold, S. [et al.]. Discrimination of TiO2 polymorphs in sedimentary and metamorphic rocks. "Contributions to mineralogy and petrology", 13 Juliol 2010, vol. 161, núm. 4, p. 581-596.
dc.identifier.issn0010-7999
dc.identifier.urihttp://hdl.handle.net/2117/12306
dc.description.abstractInvestigation by Raman spectroscopy of samples from different geological settings shows that the occurrence of TiO2 polymorphs other than rutile can hardly be predicted, and furthermore, the occurrence of anatase is more widespread than previously thought. Metamorphic pressure and temperature, together with whole rock chemistry, control the occurrence of anatase, whereas variation of mineral assemblage characteristics and/or fluid occurrence or composition takes influence on anatase trace element characteristics and re-equilibration of relict rutiles. Evaluation of trace element contents obtained by electron microprobe in anatase, brookite, and rutile shows that these vary significantly between the three TiO2 phases. Therefore, on the one hand, an appropriation to source rock type according to Nb and Cr contents, but as well application of thermometry on the basis of Zr contents, would lead to erroneous results if no phase specification is done beforehand. For the elements Cr, V, Fe, and Nb, variation between the polymorphs is systematic and can be used for discrimination on the basis of a linear discriminant analysis. Using phase group means and coefficients of linear discriminants obtained from a compilation of analyses from samples with well-defined phase information together with prior probabilities of groupings from a natural sample compilation, one is able to calculate phase grouping probabilities of any TiO2 analysis containing at least the critical elements Cr, V, Fe, and Nb. An application of this calculation shows that for the appropriation to the phase rutile, a correct-classification rate of 99.5% is obtained. Hence, phase specification by trace elements proves to be a valuable tool besides Raman spectroscopy.
dc.format.extent16 p.
dc.language.isoeng
dc.rightsAttribution-NonCommercial-NoDerivs 3.0 Spain
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/
dc.subjectÀrees temàtiques de la UPC::Enginyeria dels materials::Materials ceràmics
dc.subjectÀrees temàtiques de la UPC::Física::Física molecular::Espectroscòpia molecular
dc.subject.lcshPetrology
dc.subject.lcshMineralogy
dc.titleDiscrimination of TiO2 polymorphs in sedimentary and metamorphic rocks
dc.typeArticle
dc.subject.lemacMineralogia
dc.subject.lemacRoques sedimentàries
dc.identifier.doi10.1007/s00410-010-0551-x
dc.relation.publisherversionhttp://www.springerlink.com/content/17t102jl5326555u/
dc.rights.accessOpen Access
drac.iddocument3327103
dc.description.versionPostprint (published version)
upcommons.citation.authorTriebold, S.; Luvizotto, G.L.; Tolosana-Delgado, R.; Zack, T.; von Eynatten, H.
upcommons.citation.publishedtrue
upcommons.citation.publicationNameContributions to mineralogy and petrology
upcommons.citation.volume161
upcommons.citation.number4
upcommons.citation.startingPage581
upcommons.citation.endingPage596


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