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dc.contributor.authorLaukamp, Carsten
dc.contributor.authorAngerer, Thomas
dc.contributor.editorPhilipp, Sonja
dc.contributor.editorLeiss, Bernd
dc.contributor.editorVollbrecht, Axel
dc.contributor.editorTanner, David
dc.contributor.editorGudmundsson, Agust
dc.date.accessioned2010-11-26T13:21:10Z
dc.date.accessioned2013-01-28T10:19:37Z
dc.date.available2010-11-26T13:21:10Z
dc.date.available2013-01-28T10:19:37Z
dc.date.issued2006-03
dc.identifier.citationPhilipp, S.; Leiss, B; Vollbrecht, A.; Tanner, D.; Gudmundsson, A. (eds.): 11. Symposium "Tektonik, Struktur- und Kristallingeologie"; 2006, Univ.-Verl. Göttingen, p. 123 - 125.
dc.identifier.isbn3-938616-40-7
dc.identifier.urihttp://hdl.handle.net/11858/00-1735-0000-0001-3421-D
dc.description.abstractStructural analysis of Paleozoic Middle and Upper Austroalpine (MAA, UAA) units of the Gurktal Nappe Complex (GNC) in combination with electron microprobe analyses of multiphase garnets reveal a complex Variscan and Alpidic tectonometamorphic evolution of the GNC. Our study is focussed on the UAA ‘Murau Nappe’ and its tectonic transition to the MAA respectively to the overlying UAA Stolzalpen Nappe. The ‘Murau Nappe’ may rather be interpreted as a major zone of imbricate thrust slices of the underlying and overlying units than a distinct nappe. The results of our study lead to a reinterpretation of the ‘Murau Nappe’ as a major shear zone generated during the Eo-Alpine thrusting of the Stolzalpen Nappe over the MAA. Concerning the central GNC we conclude, that the genetic term ‘Murau Nappe’ for the lower UAA unit between MAA and Stolzalpen Nappe is not valid. Instead, its reinterpretation as a major shear zone (‘Murau shear zone’), genetically belonging to the MAA, generated during Eo-Alpine overthrusting of the Stolzalpen Nappe, is favoured. The Mesozoic Stangalm unit is interpreted as a local sequence imbricated during the northward movement of the MAA units.
dc.format.mimetypeapplication/pdf
dc.language.isodeu
dc.publisherUniversitätsverlag Göttingen
dc.relation.ispartof11. Symposium "Tektonik, Struktur- und Kristallingeologie"
dc.subject.ddc551
dc.subject.gokVEB 163
dc.subject.gokVAE 400
dc.subject.gokVKB 291
dc.subject.gokVAE 811
dc.titleEo-Alpine imbrication of Middle Austroalpine units in the Gurktal Alps, Carinthia — questioning the existence of the Upper Austroalpine Murau Nappe
dc.typeanthologyArticle
dc.subject.gokverbalZentrale Ostalpen {Geologie}
dc.subject.gokverbalTektogenese {Geologie}
dc.subject.gokverbalMetamorphe Komplexe, Alpen {Petrologie}
dc.subject.gokverbalAlpidische Orogene {Geologie}
dc.bibliographicCitation.firstPage123
dc.bibliographicCitation.lastPage125
dc.identifier.doi10.23689/fidgeo-1832
dc.type.versionpublishedVersion
dc.subject.freeGurktaler Decke
dc.subject.freeAlpidische Gebirgsbildung
dc.subject.freeTektogenese
dc.subject.freeMetamorphose <Geologie>
dc.relation.collectionGeologische Wissenschaften
dc.description.typeconference


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