Two generations of Variscan garnet: Implications from a petrochronological study of a high-grade Avalonia-derived paragneiss from the Drosendorf unit,Bohemian Massif |
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| Institution: | 1. Integrated Terrane Analysis Research (ITAR), 18 Cambridge Rd, Aldgate, 5154, SA, Australia;2. Department of Geological Sciences, University of Florida, Gainesville, FL 32611, USA;3. School of Earth Sciences, University of Tasmania, Hobart, Tasmania, Australia;4. Department of Geology, University of Adelaide, Adelaide 5005, Australia;5. Geological Survey of Western Australia, 100 Plain Street, East Perth 6004, Australia;6. Adelaide Microscopy, University of Adelaide, Adelaide 5005, Australia;1. Czech Geological Survey, 11821 Praha 1, Czech Republic;2. Université de Strasbourg, CNRS, Institut de Physique du Globe de Strasbourg, UMR 7516, 67084 Strasbourg, France;3. Institute of Geophysics ASCR, v.v.i., Boční II/1401, Prague 4 14131, Czech Republic;4. Department of Earth Science, University of California, Santa Barbara, CA 93106, USA |
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| Abstract: | Garnets in metapelitic paragneisses from the southern Drosendorf unit in the Austrian part of the Bohemian Massif exhibit two episodes of growth during the Variscan orogeny, which can be distinguished on textural and chemical grounds. The first garnet (grt1) records evidence of high-grade metamorphism in the Late Devonian (Frasnian–Famennian), while the second garnet (grt2) formed by a second high-grade event in the Early Carboniferous (Visean). Both garnet generations contain abundant inclusions, of which monazite, rutile and crystallised melt droplets are particularly useful for reconstructing P–T–t conditions. The Late Devonian age (373 ± 9 Ma) for the first episode of garnet growth was obtained from chemical dating of monazite inclusions in grt1. Metamorphic conditions during the first episode of garnet growth are estimated to have been between 0.7 and 0.8 GPa at 680–700 °C and 0.95–1.10 GPa at 745–785 °C. There followed a phase of cooling and exhumation, after which the second garnet (grt2) were formed beginning under amphibolite facies conditions and continuing prograde to peak conditions of 0.95–1.10 GPa and 745–785 °C, which are similar to those of the first garnet forming event. Subsequently, the rocks experienced near isothermal decompression to 0.5–0.8 GPa. Chemical dating of both monazite inclusions in grt2 and the matrix provide a Visean age (343 ± 3 Ma).A study of detrital zircons in these paragneisses revealed zircon forming events at around 1.2, 1.5 and 1.8 Ga, suggesting an Avalonian provenance. The lack of zircons younger than 1 Ga and the presence of Cadomian metamorphic monazite relics (652 ± 15 Ma) indicates an Early Neoproterozoic deposition age for the sedimentary protolith likely. Our documentation of a Late Devonian high-grade metamorphic event in rocks derived from Avalonian corroborates tectonic models which assume that frontal parts of the Armorican terrane had already docked with Avalonia by this time. |
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