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U/Pb dating of acid volcanism and granitoids in the Iberian Pyrite Belt (South Portuguese Zone)

dc.contributor.authorDunning, G. R.
dc.contributor.authorDíez Montes, Alejandro
dc.contributor.authorMatas, J.
dc.contributor.authorMartín Parra, L. M.
dc.contributor.authorAlmarza, J.
dc.contributor.authorDonaire, M.
dc.date.accessioned2014-11-18T11:07:11Z
dc.date.available2014-11-18T11:07:11Z
dc.date.issued2002
dc.identifier.urihttp://hdl.handle.net/10272/9325
dc.description.abstractThree samples have been analyzed, two of them belong to the volcanic ones from the IPB and a third to the rocks plutonics of the BSN. The age belonging to the granitoid of Campofrio is of 354,4 +5/-4 m.y. The ages obtained for the volcanic materials are of 347,5 ± 7,5 m.y. for the sample of Zufre and of 353 ± 2 m.y. for the rhyolltes of the SE of Nerva. Being based on the scales of the geological time, this interval of ages correspond to the Tournaisian, and moreover, suggests that the intrusion of the Sierra Norte and Be/a batholiths happen at the same time. These ages also coincide with the ages obtained for the main event of the volcanism that the IPB generates. Therefore, you can conclude that both types of rocks (volcanics and plutonics) they were formed at the same timeen_US
dc.language.isospaen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherIberian Pyrite Belten_US
dc.subject.otherSouth Portuguese Zoneen_US
dc.subject.otherVolcanismen_US
dc.subject.otherPlutonismen_US
dc.subject.otherU-Pb datingen_US
dc.subject.otherZirconen_US
dc.titleGeocronología U/Pb del volcanismo ácido y granitoides de la Faja Pirítica Ibérica (Zona Surportuguesa)en_US
dc.titleU/Pb dating of acid volcanism and granitoids in the Iberian Pyrite Belt (South Portuguese Zone)eng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessen_US


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