Fig. 7From: Reassessing the intrusive tempo and magma genesis of the late Variscan Aar batholith: U–Pb geochronology, trace element and initial Hf isotope composition of zircontaken from Table F5, age uncertainties represent “extended error”, see the Methods section for more information. Data taken from Schaltegger & Corfu (1992) are in grey; an estimated age error of ± 2 Ma has been adopted.Initial Hf isotope composition of zircon from the four intrusive pulses of the Aar batholith, determined by LA-MC-ICP-MS. Color coding is identical to Fig. 6a; εHf uncertainties areBack to article page