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The Cadomian late-orogenic alkaline magmatism in the Ossa-Morena Zone (Iberian Massif): preliminary cartography, petrography, and geochemistry of the Almedral massif

dc.contributor.authorSánchez Carretero, R.
dc.contributor.authorCarracedo Sánchez, Manuel
dc.contributor.authorEguiluz, Luis
dc.contributor.authorAlonso Olazabal, Ainhoa
dc.date.accessioned2015-03-13T12:15:51Z
dc.date.available2015-03-13T12:15:51Z
dc.date.issued1999
dc.identifier.urihttp://hdl.handle.net/10272/10095
dc.description.abstractThe Almendral massif is located in the north-western branch of the Olivenza-Monesterio antiform (Ossa Morena Zone, Iberian Massif, Spain). The pluton is composed by gabbros, sienites and alkaline granites which define an alkaline/transitional association. This magmatism marks the transition between the Cadomian orogenic regime and the Pre-Hercynian intracontinental rift for this sectoren_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.otherOssa Morena Zoneen_US
dc.subject.otherAlkaline/transitional magmatismen_US
dc.subject.otherCadomian late-orogenic alkaline stageen_US
dc.titleMagmatismo alcalino tardicadomiense en la zona de Ossa Morena (Macizo Ibérico): Cartografía, petrografía y geoquímica preliminar del Macizo de Almendralen_US
dc.titleThe Cadomian late-orogenic alkaline magmatism in the Ossa-Morena Zone (Iberian Massif): preliminary cartography, petrography, and geochemistry of the Almedral massifeng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessen_US


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