Jiménez, R.Carracedo Sánchez, ManuelOrtega, Luis ÁngelLarrea Bilbao, F. J.Alonso Olazabal, Ainhoa2014-12-122014-12-122001http://hdl.handle.net/10272/9518The Los Pedroches batholith (Iberian Massif, SW Spain) is composed by a large granodioritic intrusion and smaller monzogranitic plutons. This batholith is cross cut by a dyke complex of lamprophyres, trachyandesites, dacites, aplites, aplopegmatites, dykes of quartz and rhyolites. This last type of rocks has been studied in this paper from the cartographic and petrological point of view, recognizing five different types, according to observed texturesspaAtribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/Rhyolite dykesLos Pedroches batholithCentral Iberian ZoneLate-Hercynian magmatismjournal articleopen access