Data for: Monazite geochronology in melt-percolated UHP meta-granitoids: an example from the Erzgebirge continental subduction wedge, Bohemian Massif
S2 (Supp. Info. File No.1). Concentration (in ppm) of selected elements for the analyzed spots measured by LASS in monazite grains. Europium anomaly is indicated by “Eu*“, corresponding 207Pb-corrected 238U/206Pb dates are specified in column “age7corr”. The Eu anomaly (Eu*) was calculated using the equation Eu*=log(EuN )−((log(GdN)+log(SmN))/2) (e.g. Gordon et al., 2013).