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dc.contributor.authorHauten, Sarah
dc.contributor.authorHandy, Mark R.
dc.contributor.authorDobmeier, Christoph
dc.contributor.editorPhilipp, Sonja
dc.contributor.editorLeiss, Bernd
dc.contributor.editorVollbrecht, Axel
dc.contributor.editorTanner, David
dc.contributor.editorGudmundsson, Agust
dc.date.accessioned2010-11-26T13:21:18Z
dc.date.accessioned2013-01-28T10:19:50Z
dc.date.available2010-11-26T13:21:18Z
dc.date.available2013-01-28T10:19:50Z
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. 84 - 85.
dc.identifier.isbn3-938616-40-7
dc.identifier.urihttp://hdl.handle.net/11858/00-1735-0000-0001-343C-4
dc.description.abstractGranitic gneisses of the Central Aar Granite host a shear zone network that formed at greenschist facies conditions. The work area is located in the Bächlital (Grimsel area, Central Switzerland) and was chosen for the analysis of shear zones because of the weakly anisotropic fabric of the host gneisses. Contrary to previous publications (e.g. Choukroune & Gapais, 1983), none of these host rocks are undeformed. They contain a penetrative foliation (S1) that strikes consistently ENE-WSW with a steep dip of around 70° to the south. This foliation is overprinted by the aforementioned shear zone network, which was the main focus of this study...
dc.format.mimetypeapplication/pdf
dc.language.isodeu
dc.publisherUniversitätsverlag Göttingen
dc.relation.ispartof11. Symposium "Tektonik, Struktur- und Kristallingeologie"
dc.subject.ddc551
dc.subject.gokVAE 140
dc.subject.gokVKA 200
dc.subject.gokVKB 291
dc.subject.gokVEB 168
dc.subject.gokVKB 230
dc.subject.gokVKB 270
dc.titleFeldspar deformation in greenschist facies shear zones (Aar-Massif, Switzerland)
dc.typeanthologyArticle
dc.subject.gokverbalGesteinsdeformation {Strukturgeologie}
dc.subject.gokverbalGefügekunde der Gesteine
dc.subject.gokverbalMetamorphe Komplexe, Alpen {Petrologie}
dc.subject.gokverbalSchweizer Alpen {Geologie}
dc.subject.gokverbalMetamorphite aus sauren bis intermediären Edukten {Petrologie}
dc.subject.gokverbalProdukte mechanischer Deformation {Petrologie}
dc.bibliographicCitation.firstPage84
dc.bibliographicCitation.lastPage85
dc.identifier.doi10.23689/fidgeo-1848
dc.type.versionpublishedVersion
dc.subject.freeAarmassiv
dc.subject.freeScherzone
dc.subject.freeGranitgneis
dc.subject.freeFeldspäte
dc.subject.freeDeformation <Geologie>
dc.relation.collectionGeologische Wissenschaften
dc.description.typeconference


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