Data for: Monazite geochronology in melt-percolated UHP meta-granitoids: an example from the Erzgebirge continental subduction wedge, Bohemian Massif
Published: 10 October 2020| Version 1 | DOI: 10.17632/9xmprzzp86.1
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).