Sánchez Carretero, R.Carracedo Sánchez, ManuelEguiluz, LuisAlonso Olazabal, Ainhoa2015-03-132015-03-131999http://hdl.handle.net/10272/10095The 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 sectorspaAtribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/Ossa Morena ZoneAlkaline/transitional magmatismCadomian late-orogenic alkaline stagejournal articleopen access