Rut Jiménez San Pedro, Manuel Carracedo Sánchez, Luis Ángel Ortega Cuesta, Francisco José Larrea Bilbao, Ainhoa Alonso Olazabal
The 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 textures
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