The lowest major tectonic unit of the Tauern Window is the Venediger Nappe system, prominently exposed in the centers of the eastern and western subdomes (ETD and WTD, respectively; Fig.1). Following, e.g., Lammerer (1986), the Venediger Nappe system is interpreted to be derived from t...
The lowest major tectonic unit of the Tauern Window is the Venediger Nappe system, prominently exposed in the centers of the eastern and western subdomes (ETD and WTD, respectively; Fig.1). Following, e.g., Lammerer (1986), the Venediger Nappe system is interpreted to be derived from t...
Pre-Alpine HT relics in the EM suggest granulite (0.6–0.9 GPa, ~850 °C) and retrograde amphibolite conditions (0.5–0.3 GPa, 570–670 °C; Lardeaux and Spalla1991; Rebay and Spalla2001). A similar pre-Alpine metamorphic history was described for the 2DK by Dal Piaz et al. (1971) ...
accelerated subsidence and magmatic activity, which was related to the westward propagation of this ocean (Meliata-Maliac-Vardar; Schmid et al.2008and references therein). The horst-and-graben structure was partly obscured by prograding carbonate platforms and was finally...