Articles | Volume 36, issue 6
https://doi.org/10.5194/ejm-36-943-2024
https://doi.org/10.5194/ejm-36-943-2024
Research article
 | 
27 Nov 2024
Research article |  | 27 Nov 2024

Pressure–temperature–time and REE mineral evolution in low- to medium-grade polymetamorphic units (Austroalpine Unit, Eastern Alps)

Marianne Sophie Hollinetz, Benjamin Huet, David A. Schneider, Christopher R. M. McFarlane, Ralf Schuster, Gerd Rantitsch, Philip Schantl, Christoph Iglseder, Martin Reiser, and Bernhard Grasemann

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This preprint is open for discussion and under review for Geochronology (GChron).
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Cited articles

Bestel, M., Gawronski, T., Abart, R., and Rhede, D.: Compositional zoning of garnet porphyroblasts from the polymetamorphic Wölz Complex, Eastern Alps, Miner. Petrol., 97, 173–188, https://doi.org/10.1007/s00710-009-0084-z, 2009. 
Bollinger, L. and Janots, E.: Evidence for Mio-Pliocene retrograde monazite in the Lesser Himalaya, far western Nepal, Eur. J. Mineral., 18, 289–297, https://doi.org/10.1127/0935-1221/2006/0018-0289, 2006. 
Bojar, H. P., Bojar, A. V., Mogessie, A., Fritz, H., and Thalhammer, O. A. R.: Evolution of veins and sub-economic ore at Strassegg, Paleozoic of Graz, Eastern Alps, Austria: evidence for local fluid transport during metamorphism, Chem. Geol., 175, 757–777, https://doi.org/10.1016/S0009-2541(00)00342-9, 2001. 
Boston, K. R., Rubatto, D., Hermann, J., Engi, M., and Amelin, Y.: Geochronology of accessory allanite and monazite in the Barrovian metamorphic sequence of the Central Alps, Switzerland, Lithos, 286, 502–518, https://doi.org/10.1016/j.lithos.2017.06.025, 2017. 
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In situ U–Th–Pb dating of allanite and monazite provides a robust record of polymetamorphism in greenschist facies metapelites in the Austroalpine Unit. Variations in bulk rock Ca, Al and Na contents produced a wide range of REE-mineral-phase relationships and microstructures, making them excellent geochronometers in complex tectonic settings. Our new pressure, temperature, time and deformation data reveal Permian metamorphism and a major crustal-scale Cretaceous detachment.
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