dc.contributor.author | Klimczak, Christian | |
dc.contributor.author | Riller, Ulrich | |
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 | 2010-11-26T13:21:17Z | |
dc.date.accessioned | 2013-01-28T10:20:03Z | |
dc.date.available | 2010-11-26T13:21:17Z | |
dc.date.available | 2013-01-28T10:20:03Z | |
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. 111 - 112. | |
dc.identifier.isbn | 3-938616-40-7 | |
dc.identifier.uri | http://hdl.handle.net/11858/00-1735-0000-0001-3438-C | |
dc.description.abstract | The synformal geometry of the 1.85Ga
Sudbury Igneous Complex (SIC), an impact
melt sheet resulting from largemagnitude
meteorite impact, attests to
post-impact deformation. However, in
contrast to the overlying Onaping Formation,
a heterolithic impact melt breccia,
the SIC shows little evidence for
pervasive ductile strain. This pertains
in particular to its NE-lobe characterized
by a curvature of about 100° in
plain view. This curvature has been interpreted
either as a fold or as a primary
feature. In order to test these scenarios,
a detailed structural analysis was conducted
in the core of the NE-lobe, which
consists of rocks of the Onaping Formation... | |
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 | VKB 280 | |
dc.subject.gok | VKB 295 | |
dc.subject.gok | VAE 140 | |
dc.subject.gok | VEV 127 | |
dc.subject.gok | VKA 200 | |
dc.title | Deformation of the Onaping Formation in the NE-lobe of the Sudbury Igneous Complex, Canada: Evidence for fold adjustment flow in the core of a km-scale fold | |
dc.type | anthologyArticle | |
dc.subject.gokverbal | Impaktgesteine {Petrologie} | |
dc.subject.gokverbal | Metamorphe Komplexe, Nordamerika {Petrologie} | |
dc.subject.gokverbal | Gesteinsdeformation {Strukturgeologie} | |
dc.subject.gokverbal | Ontario {Geologie} | |
dc.subject.gokverbal | Gefügekunde der Gesteine | |
dc.bibliographicCitation.firstPage | 111 | |
dc.bibliographicCitation.lastPage | 112 | |
dc.identifier.doi | 10.23689/fidgeo-1863 | |
dc.type.version | publishedVersion | |
dc.subject.free | Sudbury <Ontario. Region> | |
dc.subject.free | Mehrfachringbassin | |
dc.subject.free | Proterozoikum | |
dc.subject.free | Impaktmetamorphes Gestein | |
dc.subject.free | Deformation <Geologie> | |
dc.relation.collection | Geologische Wissenschaften | |
dc.description.type | conference | |