dc.contributorUniversidade Federal do Rio Grande do Sul (UFRGS)
dc.contributorUniversidade Estadual Paulista (Unesp)
dc.contributorUniversidade Estadual de Campinas (UNICAMP)
dc.date.accessioned2014-05-20T13:23:13Z
dc.date.available2014-05-20T13:23:13Z
dc.date.created2014-05-20T13:23:13Z
dc.date.issued2010-02-01
dc.identifierRevista Mexicana de Fisica. Coyoacan: Soc Mexicana Fisica, v. 56, n. 1, p. 16-21, 2010.
dc.identifier0035-001X
dc.identifierhttp://hdl.handle.net/11449/6966
dc.identifierWOS:000275031400005
dc.description.abstractAges of zircon from sedimentary samples of Rio Parana Formation, belonging of Bauru Group, north of Parana Basin, Brazil, has been determined by zircon Fission Track and U-Th-Pb in situ dating methods. The obtained ages are from same zircon grain that provided information on the source areas for the sediments and the morphotectonic events.
dc.languageeng
dc.publisherSoc Mexicana Fisica
dc.relationRevista Mexicana de Fisica
dc.relation0.595
dc.rightsAcesso aberto
dc.sourceWeb of Science
dc.subjectZircon, fission track method
dc.subjectU-Th-Pb in situ dating
dc.subjectBauru Group
dc.subjectRio Parana Formation
dc.titleZircon fission track and U-Th-Pb in situ dating of Rio Parana Formation, Parana Basin, Brazil
dc.typeArtículos de revistas


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