The metamorphic evolution of migmatites from the Otztal Complex (Tyrol, Austria) and constraints on the timing of the pre-Variscan high-T event in the Eastern Alps

Within the Otztal Complex (OC), migmatites are the only geological evidence of the pre-Variscan metamorphic evolution, which led to the occurrence Of partial anatexis in different areas of the complex. We investigated migmatites from three localities in the OC, the Winnebach migmatite in the central part and the Verpeil- and Nauderer Gaisloch migmatite in the western part. We determined metamorphic stages using textural relations and electron microprobe analyses. Furthermore, chemical microprobe ages of monazites were obtained in order to associate the inferred stages of mineral growth to metamorphic events. All three migmatites show evidence for a polymetamorphic evolution (pre-Variscan, Variscan) and only the Winnebach migmatite shows evidence for a P-accentuated Eo-Alpine metamorphic overprint in the central OC. The P-T data range from 670-750 degrees C and <2.8 kbar for the pre-Variscan event, 550-650 degrees C and 4-7 kbar for the Variscan event and 430-490 degrees C and ca. 8.5 kbar for the P-accentuated Eo-Alpine metamorphic overprint. U-Th-Pb electron microprobe dating of monazites from the leucosomes from all three migmatites provides an average age of 441 +/- 18 Ma, thus indicating a pervasive Ordovician-Silurian metamorphic event in the OC.