Alonso Olazabal, AinhoaOrtega, Luis ÁngelMenéndez, M.Carracedo Sánchez, ManuelAranguren, A.2014-11-032014-11-032003http://hdl.handle.net/10272/9073A Rb-Sr whole-rock array corresponding to a circa age of304 ± 6 Ma has been obtained for the peraluminous granite of Campanario - La Haba pluton. The Sr initial ratio of 0.70619 ± 0.00034 of this pluton is less radiogenic than those typical S granites of metasedimentary crustal origin, indicating that this granite may not have been exclusively derived from crustal sources. The emplacement occurred during late-Hercynian deformation eventsspaAtribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/Peraluminous graniteGranitic unit of the Los Pedroches batholithGeochronologyIsotope geochemistryExtremadurajournal articleopen access