HT–LP crustal syntectonic anatexis as a source of the Permian magmatism in the Eastern Southern Alps: evidence from xenoliths in the Euganean trachytes (NE Italy).
The whole-rock geochemistry and zircon Hf-O isotopic data, zircon U-Pb dating, major and trace elements chosen for thermodynamic simulations and trace element characteristics modelling in the study. T
