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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.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.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.subject.otherCentral Iberian Zoneen_US
dc.subject.otherAlmadén areaen_US
dc.subject.otherLos Pedroches batholithen_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

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