Characterization of polymetamorphism in the Austroalpine basement east of the Tauern Window using garnet isopleth thermobarometry

Garnet in metapelites from the Wolz and Rappold Complexes of the Austroalpine basement east of the Tauern Window typically shows two distinct growth zones. A first garnet generation usually forms the cores of garnet porphyroblasts and is separated by a prominent microstructural and chemical discontinuity from a second garnet generation, which forms rims of variable width. Whereas the rims were formed during the Eo-Alpine metamorphic overprint, the garnet cores represent remnants of at least two pre-Eo-Alpine metamorphic events. The pressure and temperature estimates obtained from garnet isopleth thermobarometry applied to the first growth increments of the pre-Eo-Alpine garnet cores from the Wolz and Rappold Complexes cluster into two distinct domains: (i) in the Wolz Complex, incipient growth of the first-generation garnet occurred at 4 +/- 0.5 kbar and 535 +/- 20 degrees C, (ii) in the Rappold Complex, incipient growth of the oldest garnet cores took place at 5.3 +/- 0.3 kbar and 525 +/- 15 degrees C. The Eo-Alpine garnet generation started to grow at 6.5 +/- 0.5 kbar and 540 +/- 10 degrees C. According to radiometric dating, the low-pressure garnet from the Wolz complex was formed during a Permian metamorphic event. The first-generation garnet of the Rappold Complex is probably of Variscan age.