Thermobarometric constraints on pressure variations across the Plattengneiss shear zone of the Eastern Alps: implications for exhumation models during Eoalpine subduction
Author:
Affiliation:
1. Earth System Science Research Centre; Institute for Geosciences; University of Mainz; Becherweg 21 D-55099 Mainz Germany
2. Department of Earth Science; University of Graz; Universitätsplatz 2 A-8010 Graz Austria
Publisher
Wiley
Subject
Geochemistry and Petrology,Geology
Link
http://onlinelibrary.wiley.com/wol1/doi/10.1111/jmg.12069/fullpdf
Reference52 articles.
1. Slab breakoff: a model for syncollisional magmatism and tectonics in the Alps;Blanckenburg;Tectonics,1995
2. Pseudosection modelling for a selected eclogite body from the Koralpe (Hohl), Eastern Alps;Bruand;Mineralogy and Petrology,2009
3. Petrology, geochronology and tectonics of shear zones in the Zermatt-Saas and Combin zones of the Western Alps;Cartwright;Journal of Metamorphic Geology,2002
4. A mechanism for syn-collisional deep rock exhumation and associated normal faulting: results from physical modelling;Chemenda;Earth and Planetary Science Letters,1995
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1. H2O-fluxed melting of eclogite during exhumation: an example from the eclogite type-locality, Eastern Alps (Austria);Lithos;2021-06
2. Tectonic interpretation of the metamorphic field gradient south of the Koralpe in the Eastern Alps;Austrian Journal of Earth Sciences;2018-12-01
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4. Details of the gabbro-to-eclogite transition determined from microtextures and calculated chemical potential relationships;Journal of Metamorphic Geology;2016-10-14
5. The Plankogel detachment of the Eastern Alps: petrological evidence for an orogen-scale extraction fault;Journal of Metamorphic Geology;2016-01-21
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