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Campanario-La Haba pluton tipology: petrogenetic implications

dc.contributor.authorAlonso Olazabal, Ainhoa
dc.contributor.authorAranguren, A.
dc.contributor.authorCarracedo Sánchez, Manuel
dc.contributor.authorLarrea Bilbao, F. J.
dc.date.accessioned2016-06-22T09:18:59Z
dc.date.available2016-06-22T09:18:59Z
dc.date.issued1996
dc.identifier.urihttp://hdl.handle.net/10272/12408
dc.description.abstractThe Campanario-La Haba pluton is located in the suothern part of the Central-Iberian Zone. It is a coarse-grained 5 type granitoid with cordierite. Typologicaly, this pluton is a peraluminous granitoid , CCA type. Mineralogy and petrologycally, the Campanario-La Haba pluton is closer to the Central Extremadura Bath olith ( Cabeza de Araya type) than to the granitic unit of the Los Pedrodres Batholith (Sta. Eufemia, El Guijo, Cerro Mogabar, Cardeña)en_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.otherCoarse grained peraluminous granitoiden_US
dc.subject.other5 type granitoid ,en_US
dc.subject.otherCCA typeen_US
dc.subject.otherPetrogenesisen_US
dc.titleTipología del plutón de Campanario-La Haba: implicaciones petrogenéticasen_US
dc.titleCampanario-La Haba pluton tipology: petrogenetic implicationseng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessen_US


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