Data for: Monazite geochronology in melt-percolated UHP meta-granitoids: an example from the Erzgebirge continental subduction wedge, Bohemian Massif

Published: 10-10-2020| Version 1 | DOI: 10.17632/nkgv74nczj.1
Prokop Zavada


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).