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High-K calc-alkaline granitoid rocks in the Central Iberian Zone: the Garlitos-El Borracho area

dc.contributor.authorDonaire Romero, Teodosio 
dc.contributor.authorPascual Martínez, Emilio 
dc.contributor.authorHigueras, Pablo L.
dc.contributor.authorMorata Céspedes, Diego
dc.date.accessioned2016-06-20T12:39:59Z
dc.date.available2016-06-20T12:39:59Z
dc.date.issued1996
dc.identifier.urihttp://hdl.handle.net/10272/12396
dc.description.abstractNew petrographic and chemical data on the Garlitos pluton and other associated igneous rocks in the Almadén area have shown a high-K calc-alkaline character and clear simiarities with other calc-alkaline granitoids, in particular the lithotypes dominant in the Los Pedroches batholith. Similarities include petrographical, mineralogical and chemical features, as well as a number of metamorphic xenoliths, suggesting that igneous rocks were generated from similar sources and emplaced through similar crustal segments.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.otherCentral Iberian Zoneen_US
dc.subject.otherAlmadén areaen_US
dc.subject.otherLos Pedroches batholithen_US
dc.subject.otherGranodioriteen_US
dc.subject.otherOrthopyroxeneen_US
dc.subject.otherXenolithsen_US
dc.titleRocas granitoides calcoalcalinas altas en potasio en la Zona Centroibérica: el área Garlitos-El Borrachoen_US
dc.titleHigh-K calc-alkaline granitoid rocks in the Central Iberian Zone: the Garlitos-El Borracho areaeng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessen_US


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