“…With the advance of low-temperature thermochronology since the late 80´s, a growing number of zircon and apatite fission track data (ZFT and AFT, respectively) helped to resolve processes in the deeper levels of the upper crust (e.g. Wagner et al, 1977;Grundmann and Morteani, 1985;Staufenberg, 1987;Hejl, 1997Hejl, , 1998Dunkl et al, 2003;Foeken et al, 2007;Wölfler et al, 2008Wölfler et al, , 2012. And finally, the (U-Th)/He methods available since the beginning of this century allowed scientists to track shallow crystal processes operating at temperatures <100C° in the shallowest levels of the upper crust (e.g.…”