dc.contributorCNR
dc.contributorUniversidade Estadual de Campinas (UNICAMP)
dc.contributorUniv Pavia
dc.contributorUniversidade Estadual Paulista (Unesp)
dc.contributorUniv Nacl Salta
dc.date.accessioned2014-05-20T13:22:56Z
dc.date.accessioned2022-10-05T13:09:14Z
dc.date.available2014-05-20T13:22:56Z
dc.date.available2022-10-05T13:09:14Z
dc.date.created2014-05-20T13:22:56Z
dc.date.issued2007-06-01
dc.identifierGeostandards and Geoanalytical Research. Malden: Wiley-blackwell, v. 31, n. 2, p. 105-124, 2007.
dc.identifier1639-4488
dc.identifierhttp://hdl.handle.net/11449/6828
dc.identifier10.1111/j.1751-908X.2007.00844.x
dc.identifierWOS:000247205300004
dc.identifier1543738193935256
dc.identifier.urihttp://repositorioslatinoamericanos.uchile.cl/handle/2250/3883880
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.
dc.languageeng
dc.publisherWiley-Blackwell
dc.relationGeostandards and Geoanalytical Research
dc.relation3.929
dc.relation1,430
dc.rightsAcesso restrito
dc.sourceWeb of Science
dc.subjectfission-track dating
dc.subject(40)Ar/(39)Ar dating
dc.subjectnatural glasses
dc.subjectage standards
dc.titleNew constraints on ages of glasses proposed as reference materials for fission-track dating
dc.typeArtigo


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