Timing of metamorphism in the Tauern Window, Eastern Alps: Rb‐Sr ages and fabric formation

Abstract

ABSTRACTThe Peripheral Schieferhülle of the Tauern Window of the Eastern Alps represents post‐Hercynian Penninic cover sequences and preserves a record of metamorphism in the Alpine orogeny, without the inherited remnants of Hercynian events that are retained in basement rocks. The temperature‐time‐deformation history of rocks at the lower levels of these cover sequences have been investigated by geochronological and petrographic study of units whose P‐T evolution and structural setting are already well understood.The Eclogite Zone of the central Tauern formed from protoliths with Penninic cover affinities, and suffered early Alpine eclogite facies metamorphism before tectonic interposition between basement and cover. It then shared a common metamorphic history with these units, experiencing blueschist facies and subsequent greenschist facies conditions in the Alpine orogeny. The greenschist facies phase, associated with penetrative deformation in the cover and the influx of aqueous fluids, reset Sr isotopes in metasediments throughout the eclogite zone and cover schists, recording deformation and peak metamorphism at 28‐30 Ma.The Peripheral Schieferhülle of the south‐east Tauern Window yields Rb‐Sr white mica ages which can be tied to the structural evolution of the metamorphic pile. Early prograde fabrics pre‐date 31 Ma, and were reworked by the formation of the large north‐east vergent Sonnblick fold structure at 28 Ma. Peak metamorphism post‐dated this deformation, but by contrast to the equivalent levels in the central Tauern, peak metamorphic conditions did not lead to widespread homogenization of the Sr isotopes. Localized deformation continued into the cooling path until at least 23 Ma, partially or wholly resetting Sr white mica ages in some samples.These isotopic ages may be integrated with structural data in regional tectonic models, and may constrain changes in the style of crustal deformation and plate interaction. However, such interpretations must accommodate the demonstrable variation in thermal histories over small distances.