Replication Data for: Widespread evidence of mid-Permian magmatic activity related to rifting following the Variscan orogeny (Inner Western Carpathians)

Table S1. Excel spreadsheet of the zircon geochronological data obtained using SIMS.
Table S2. Excel spreadsheet of the zircon geochronological data obtained using LA-ICP-MS.
Table S3. Summary of the whole-rock geochemical analysis of samples from the Betliar Pluton.
Table S4. Summary of the whole-rock geochemical analysis of samples from the Klenovec Pluton.
Figure S1. X-ray Diffraction (XRD) data from serpentinized samples collected at the TT08 locality, indicating the presence of lizardite, forsterite, and fayalite.
Figure S2. Photographs of the Gemeric and Veporic granites dated in this study.
Figure S3. Petrographic images of Betliar granite samples (A) IR19A (plane polarized light), (B) IR19A (crossed polarized light), (C) IR19B (plane polarized light), (D) IR19B (crossed polarized light).
Figure S4. Petrographic images of Betliar granite samples (A) IR19C (plane polarized light) (B) IR19C (crossed polarized light), (C) IR19D (crossed polarized light), and IR19D (crossed polarized light).
Figure S5. Petrographic images of Betliar granite samples (A) IR20A, (B) IR20B, and (C) IR20C. Panel D shows Hnilec granite sample TT51. All images are taken in crossed polarized light.
Figure S6. Panels (A) and (B) are petrographic images of Elisabeth Mine granite sample TT08 in crossed polarized light. Panels (C) and (D) show petrographic images of Klenovec granite sample TT48. Panel (C) is in plane polarized light, whereas panel (D) is in crossed polarized light.
Figure S7. Panels (A) and (B) are petrographic images of Poproč granite sample TT49. Panel (A) is in plane polarized light, whereas panel (B) is in crossed polarized light.