Tracing magma sources of three different S-type peraluminous granitoid series by in situ U-Pb geochronology and Hf isotope zircon composition: The Variscan Montes de Toledo batholith (central Spain)
Keywords: U-Pb geochronology; Hf isotope zircon composition; Peraluminous granites; Montes de Toledo batholith; Iberian Variscan Belt; S-type granitoid magma sources;