dc.contributor.author | Laukamp, Carsten | |
dc.contributor.author | Angerer, Thomas | |
dc.contributor.editor | Philipp, Sonja | |
dc.contributor.editor | Leiss, Bernd | |
dc.contributor.editor | Vollbrecht, Axel | |
dc.contributor.editor | Tanner, David | |
dc.contributor.editor | Gudmundsson, Agust | |
dc.date.accessioned | 2010-11-26T13:21:10Z | |
dc.date.accessioned | 2013-01-28T10:19:37Z | |
dc.date.available | 2010-11-26T13:21:10Z | |
dc.date.available | 2013-01-28T10:19:37Z | |
dc.date.issued | 2006-03 | |
dc.identifier.citation | Philipp, 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.isbn | 3-938616-40-7 | |
dc.identifier.uri | http://hdl.handle.net/11858/00-1735-0000-0001-3421-D | |
dc.description.abstract | Structural 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.mimetype | application/pdf | |
dc.language.iso | deu | |
dc.publisher | Universitätsverlag Göttingen | |
dc.relation.ispartof | 11. Symposium "Tektonik, Struktur- und Kristallingeologie" | |
dc.subject.ddc | 551 | |
dc.subject.gok | VEB 163 | |
dc.subject.gok | VAE 400 | |
dc.subject.gok | VKB 291 | |
dc.subject.gok | VAE 811 | |
dc.title | Eo-Alpine imbrication of Middle Austroalpine units in the Gurktal Alps, Carinthia — questioning the existence of the Upper Austroalpine Murau Nappe | |
dc.type | anthologyArticle | |
dc.subject.gokverbal | Zentrale Ostalpen {Geologie} | |
dc.subject.gokverbal | Tektogenese {Geologie} | |
dc.subject.gokverbal | Metamorphe Komplexe, Alpen {Petrologie} | |
dc.subject.gokverbal | Alpidische Orogene {Geologie} | |
dc.bibliographicCitation.firstPage | 123 | |
dc.bibliographicCitation.lastPage | 125 | |
dc.identifier.doi | 10.23689/fidgeo-1832 | |
dc.type.version | publishedVersion | |
dc.subject.free | Gurktaler Decke | |
dc.subject.free | Alpidische Gebirgsbildung | |
dc.subject.free | Tektogenese | |
dc.subject.free | Metamorphose <Geologie> | |
dc.relation.collection | Geologische Wissenschaften | |
dc.description.type | conference | |