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On epidote fission track dating

dc.contributor.authorCurvo, EAC
dc.contributor.authorHadler, J. C.
dc.contributor.authorIunes, P. J.
dc.contributor.authorGuedes, S.
dc.contributor.authorTello, CAS
dc.contributor.authorPaulo, SR
dc.contributor.authorHackspacher, P. C.
dc.contributor.authorPalissari, R.
dc.contributor.authorMoreira, PAFP
dc.contributor.institutionUniversidade Estadual de Campinas (UNICAMP)
dc.contributor.institutionUniv Fed Mato Grosso
dc.contributor.institutionUniversidade Estadual Paulista (Unesp)
dc.date.accessioned2014-05-20T15:30:09Z
dc.date.available2014-05-20T15:30:09Z
dc.date.issued2005-12-01
dc.description.abstractThe use of epidote in fission track dating was abandoned since the beginning of the 1980s due to difficulties like absence of a standard etching procedure, obtainment of different closure temperatures and the percentage of the datable samples. The results become much more reproducible when restricting fission track analysis to a peculiar kind of track. We are also studying confined track length, what makes possible to obtain information about fossil track annealing. Fission tracks in epidote were successfully etched with 48% HF at 35 degrees C for 12.5 min. Dating samples by the external detector method was not possible due to problems in measuring the efficiency factor held between the number of fossil fission tracks and tracks induced in mica. Dating a sample from Brejui, RN, Brazil with the population method gave a corrected age of 510 +/- 69Ma, in agreement with published U/Th-Pb ages. From the fact that the fossil track length histogram was bimodal, we were able to infer that this sample registered a thermal episode during its history.These preliminary results indicate that epidote deserves further studies to establish whether it can be employed as a thermochronological tool. (c) 2005 Elsevier Ltd. All rights reserved.en
dc.description.affiliationUniv Estadual Campinas, Inst Fis Gleb Wataghin, BR-13083970 Campinas, SP, Brazil
dc.description.affiliationUniv Fed Mato Grosso, UFMT, Dept Fis, Inst Ciências Exatas & Terra, BR-78060900 Cuiaba, MT, Brazil
dc.description.affiliationUniv Estadual Paulista, Inst Geociencias & Ciências Exatas, BR-13506900 Rio Claro, SP, Brazil
dc.description.affiliationUnespUniv Estadual Paulista, Inst Geociencias & Ciências Exatas, BR-13506900 Rio Claro, SP, Brazil
dc.format.extent641-645
dc.identifierhttp://dx.doi.org/10.1016/j.radmeas.2004.06.016
dc.identifier.citationRadiation Measurements. Oxford: Pergamon-Elsevier B.V., v. 39, n. 6, p. 641-645, 2005.
dc.identifier.doi10.1016/j.radmeas.2004.06.016
dc.identifier.issn1350-4487
dc.identifier.lattes1040135935908734
dc.identifier.orcid0000-0003-2125-3050
dc.identifier.urihttp://hdl.handle.net/11449/39587
dc.identifier.wosWOS:000229716600012
dc.language.isoeng
dc.publisherElsevier B.V.
dc.relation.ispartofRadiation Measurements
dc.relation.ispartofjcr1.369
dc.relation.ispartofsjr0,509
dc.rights.accessRightsAcesso restrito
dc.sourceWeb of Science
dc.subjectepidotept
dc.subjectfission track datingpt
dc.subjectbrejui epidotept
dc.subjectBorborema province-Brazilpt
dc.titleOn epidote fission track datingen
dc.typeArtigo
dcterms.licensehttp://www.elsevier.com/about/open-access/open-access-policies/article-posting-policy
dcterms.rightsHolderElsevier B.V.
unesp.author.lattes1040135935908734[7]
unesp.author.lattes5982597921345094[5]
unesp.author.orcid0000-0003-0975-6034[9]
unesp.author.orcid0000-0003-2125-3050[7]
unesp.author.orcid0000-0003-2843-775X[9]
unesp.author.orcid0000-0002-7753-8584[4]
unesp.author.orcid0000-0002-0369-8999[5]
unesp.campusUniversidade Estadual Paulista (Unesp), Instituto de Geociências e Ciências Exatas, Rio Claropt
unesp.departmentPetrologia e Metalogenia - IGCEpt

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