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Fig. 1 | Swiss Journal of Geosciences

Fig. 1

From: Electron microprobe petrochronology of monazite-bearing garnet micaschists in the Oetztal-Stubai Complex (Alpeiner Valley, Stubai)

Fig. 1

a Location of the study area in the basement units of the Central and Eastern Alps: BSTW Basement South of Tauern Window, GWZ Graywacke Zone, IL Insubric Line, IQ Innsbrucker Quartzphyllite, JL Judicarien Line, Ko Koralpe, OSC Oetztal-Stubai Complex, PL Periadriatic Lineament, Sa Saualpe, SA South Alpine, Si Silvretta, TW Tauern Window (Penninic Unit). b Geological sketch map of the Oetztal-Stubai basement in the Central Alps, redrawn after Schmidegg (1964), with the various additions by Miller et al. (1967) and Purtscheller (1978), with Variscan mineral zones and domains of Alpine Cretaceous metamorphism after Thöni (1981), Frank et al. (1987) and Hoinkes and Thöni (1993). Study area around the Franz-Senn-Hütte in the Stubai Alps (Stu) is marked by square. A Alpeiner metagranodiorite, B Bassler metagranite, CMB Central Metabasite Zone, KM Klopeiner migmatite, VM Verpeil migmatite, WM Winnebach migmatite, S Schrankogel complex with metabasites. Sampling areas in Rode et al. (2012) are Sellrain (Sel), E of Sölden (Söl), and W of Umhausen (Um) around Erlanger Hütte. Vent (V) is situated in the area with large-scale Schlingen structures

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