Please use this identifier to cite or link to this item: http://rigeo.cprm.gov.br/jspui/handle/doc/573
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dc.contributor.authorFRAGA, Lêda Maria Barreto-
dc.contributor.authorMACAMBIRA, Moacir José Buenano-
dc.contributor.authorDALL’AGNOL, Roberto-
dc.contributor.authorCOSTA, João Batista Sena Costa-
dc.date.accessioned2013-12-19T16:32:42Z-
dc.date.available2013-12-19T16:32:42Z-
dc.date.issued2009-
dc.identifier.citationFRAGA, Lêda Maria Barreto; MACAMBIRA, Moacir José Buenano; DALL’AGNOL, Roberto; COSTA, João Batista Sena Costa. 1.94-1.93 Ga charnockitic magmatism from the central part of the Guyana Shield, Roraima, Brazil: Single-zircon evaporation data and tectonic implications. Journal of South American Earth Sciences, Oxford, v.v. 27, n.4, p.247-257, Oxford.-
dc.identifier.urihttp://rigeo.cprm.gov.br/jspui/handle/doc/573-
dc.description.abstractAge and origin of the charnockitic rocks of the central part of the Guyana Shield have been a matter of discussion. These rocks have been interpreted either as Transamazonian granulites metamorphosed around 2.02 Ga or as 1.56 Ga old igneous charnockites.Recently, most of the Roraima charnockitic rocks have been recognized as igneous rocks and included into the Serra da Prata Suite (SPS). Five Pb–Pb singlezircon evaporation ages were obtained for samples representative of different facies of the SPS and these constrained the age of the charnockitic magmatism between 1943 ± 5 Ma and 1933 ± 2 Ma. This charnockitic magmatism may be related to a post-collisional setting after the evolution of the Cauarane-Coeroeni Belt ( 2.00 Ga), or may represent a post-collisional (or intracontinental?) magmatism related to orogenic activities along the plate margins around 1.95–1.94 Ga-
dc.subjectGEOCRONOLOGIA-
dc.subjectMAGMATISMO-
dc.subjectROCHAS CHARNOCKÍTICAS-
dc.subjectPALEOPROTEROZÓICO-
dc.subjectCRÁTON AMAZÔNICO-
dc.subjectBRASIL-
dc.subjectRORAIMA-
dc.title1.94-1.93 Ga charnockitic magmatism from the central part of the Guyana Shield, Roraima, Brazil: Single-zircon evaporation data and tectonic implications-
dc.typeArticle-
dc.localOxford-
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