Data for: Monazite geochronology in melt-percolated UHP meta-granitoids: an example from the Erzgebirge continental subduction wedge, Bohemian Massif
S3 (Supp. Info. File No.1). Concentration (in ppm) of selected elements for the analyzed spots measured by LASS in garnet grains (Figure 12). Europium anomaly is indicated by “Eu*“. The Eu anomaly (Eu*) was calculated using the equation Eu*=log(EuN )−((log(GdN)+log(SmN))/2) (e.g. Gordon et al., 2013).