You are in the accessibility menu

Please use this identifier to cite or link to this item: http://acervodigital.unesp.br/handle/11449/6828
Full metadata record
DC FieldValueLanguage
dc.contributor.authorLaurenzi, Marinella A.-
dc.contributor.authorBalestrieri, Maria Laura-
dc.contributor.authorBigazzi, Giulio-
dc.contributor.authorNeto, Julio C. Hadler-
dc.contributor.authorIunes, Pedro J.-
dc.contributor.authorNorelli, Pio-
dc.contributor.authorOddone, Massimo-
dc.contributor.authorOsorio Araya, Ana Maria-
dc.contributor.authorViramonte, Jose G.-
dc.date.accessioned2014-05-20T13:22:56Z-
dc.date.accessioned2016-10-25T16:44:02Z-
dc.date.available2014-05-20T13:22:56Z-
dc.date.available2016-10-25T16:44:02Z-
dc.date.issued2007-06-01-
dc.identifierhttp://dx.doi.org/10.1111/j.1751-908X.2007.00844.x-
dc.identifier.citationGeostandards and Geoanalytical Research. Malden: Wiley-blackwell, v. 31, n. 2, p. 105-124, 2007.-
dc.identifier.issn1639-4488-
dc.identifier.urihttp://hdl.handle.net/11449/6828-
dc.identifier.urihttp://acervodigital.unesp.br/handle/11449/6828-
dc.description.abstractNew analyses have been performed in order to enhance the data-set on the independent ages of four glasses that have been proposed as reference materials for fission-track dating. The results are as follows. Moldavite - repeated (40)Ar/(39)Ar age determinations on samples from deposits from Bohemia and Moravia yielded an average of 14.34 +/- 0.08 Ma. This datum agrees with other recent determinations and is significantly younger than the (40)Ar/(39)Ar age of 15.21 +/- 0.15 Ma determined in the early 1980s. Macusanite (Peru) -four K-Ar ages ranging from 5.44 +/- 0.06 to 5.72 +/- 0.12 Ma have been published previously. New (40)Ar/(39)Ar ages gave an average of 5.12 +/- 0.04 Ma. Plateau fission-track ages determined using the IRMM-540 certified glass and U and Th thin films for neutron fluence measurements agree better with these new (40)Ar/(39)Ar ages than the previously published ages. Roccastrada glass (Italy) - a new (40)Ar/(39)Ar age, 2.45 +/- 0.04 Ma, is consistent with previous determinations. The Quiron obsidian (Argentina) is a recently discovered glass that has been proposed as an additional reference material for its high spontaneous track density (around 100 000 cm(-2)). Defects that might produce spurious tracks are virtually absent. An independent (40)Ar/(39)Ar age of 8.77 +/- 0.09 Ma was determined and is recommended for this glass. We believe that these materials, which will be distributed upon request to fission-track groups, will be very useful for testing system calibrations and experimental procedures.en
dc.format.extent105-124-
dc.language.isoeng-
dc.publisherWiley-Blackwell-
dc.sourceWeb of Science-
dc.subjectfission-track datingpt
dc.subject(40)Ar/(39)Ar datingpt
dc.subjectnatural glassespt
dc.subjectage standardspt
dc.titleNew constraints on ages of glasses proposed as reference materials for fission-track datingen
dc.typeoutro-
dc.contributor.institutionCNR-
dc.contributor.institutionUniversidade Estadual de Campinas (UNICAMP)-
dc.contributor.institutionUniv Pavia-
dc.contributor.institutionUniversidade Estadual Paulista (UNESP)-
dc.contributor.institutionUniv Nacl Salta-
dc.description.affiliationCNR, Ist Geosci & Georisorse, I-56124 Pisa, Italy-
dc.description.affiliationUniv Estadual Campinas, Inst Fis, Dept Raios Cosm & Cronol, BR-13083970 Campinas, SP, Brazil-
dc.description.affiliationUniv Pavia, Dipartimento Chim Gen, I-27100 Pavia, Italy-
dc.description.affiliationUniv Estado São Paulo, UNESP, Dept Fis Quim & Biol, BR-19060900 Presidente Prudente, SP, Brazil-
dc.description.affiliationUniv Nacl Salta, Inst Geonorte, RA-4400 Salta, Argentina-
dc.description.affiliationUnespUniv Estado São Paulo, UNESP, Dept Fis Quim & Biol, BR-19060900 Presidente Prudente, SP, Brazil-
dc.identifier.doi10.1111/j.1751-908X.2007.00844.x-
dc.identifier.wosWOS:000247205300004-
dc.rights.accessRightsAcesso restrito-
dc.relation.ispartofGeostandards and Geoanalytical Research-
Appears in Collections:Artigos, TCCs, Teses e Dissertações da Unesp

There are no files associated with this item.
 

Items in DSpace are protected by copyright, with all rights reserved, unless otherwise indicated.