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dc.contributor.authorSchneider, Susanne
dc.contributor.authorRosenberg, Claudio
dc.contributor.editorPhilipp, Sonja
dc.contributor.editorLeiss, Bernd
dc.contributor.editorVollbrecht, Axel
dc.contributor.editorTanner, David
dc.contributor.editorGudmundsson, Agust
dc.date.accessioned2010-11-26T13:21:27Z
dc.date.accessioned2013-01-28T12:41:37Z
dc.date.available2010-11-26T13:21:27Z
dc.date.available2013-01-28T12:41:37Z
dc.date.issued2006-03
dc.identifier.isbn3-938616-40-7
dc.identifier.urihttp://hdl.handle.net/11858/00-1735-0000-0001-345D-9
dc.description.abstractThe working area is located in the Stillupp Valley (Tirol, Austria), where the western termination of the SEMPfault (Salzach, Ennstal, Mariazell, Puchberg), overprints the northernmost margin of the Zentralgneiss. This sinistral shearzone, which has a length of about 300 km, and causes a lateral displacement of 60km (Linzer et al. 2002), marks part of the northern border of the Tauern Window...
dc.format.mimetypeapplication/pdf
dc.language.isodeu
dc.publisherUniversitätsverlag Göttingen
dc.relation.ispartof11. Symposium "Tektonik, Struktur- und Kristallingeologie"
dc.subject.ddc551
dc.subject.gokVAE 850
dc.subject.gokVAE 400
dc.subject.gokVAE 140
dc.subject.gokVEB 161
dc.titleKinematics of the SEMPfault in the western Tauern Window (Stillupp Valley)
dc.typeanthologyArticle
dc.subject.gokverbalFestländische Lineamente {Geologie}
dc.subject.gokverbalTektogenese {Geologie}
dc.subject.gokverbalGesteinsdeformation {Strukturgeologie}
dc.subject.gokverbalOstalpen {Geologie}
dc.identifier.doi10.23689/fidgeo-1932
dc.type.versionpublishedVersion
dc.subject.freeTauernfenster <West>
dc.subject.freeScherzone
dc.subject.freeHorizontalverschiebung
dc.subject.freeTranspression
dc.relation.collectionGeologische Wissenschaften
dc.description.typeconference
dc.notes.internDas ist ein Poster! Seitenzahlen konnten nicht ermittelt werden.


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