Neiva, A.M.R.Williams, IanLima, S MTeixeira, R J S2015-12-130024-4937http://hdl.handle.net/1885/72300Late Carboniferous U-Pb ages have been measured on igneous zircon from late- and post-D 3 Sn-bearing two-mica granites from the Gouveia area in the Central Iberian Zone. Inherited zircon from these granites is mainly of Neoproterozoic age, a small amountKeywords: argon-argon dating; Cambrian; cooling; Devonian-Carboniferous boundary; emplacement; Gondwana; granite; Hercynian orogeny; muscovite; Ordovician-Silurian boundary; Proterozoic; recrystallization; uranium-lead dating; Central Iberian Zone; Portugal Emplacement ages; Inheritance; Muscovite; Recrystallization/cooling ages; ZirconU-Pb and Ar-39/Ar-40 data constraining the ages of the source, emplacement and recrystallization/cooling events from late- to post-D-3 Variscan granites of the Gouveia area, central Portugal201210.1016/j.lithos.2012.02.0122016-02-24