dc.contributor.author | Steenken, André | |
dc.contributor.author | Siegesmund, Siegfried | |
dc.contributor.author | Luchi, Mónica G. López de | |
dc.contributor.author | Rapalini, Augusto | |
dc.contributor.author | Wemmer, Klaus | |
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 | 2010-11-26T13:21:25Z | |
dc.date.accessioned | 2013-01-28T10:20:22Z | |
dc.date.available | 2010-11-26T13:21:25Z | |
dc.date.available | 2013-01-28T10:20:22Z | |
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. 216 - 220. | |
dc.identifier.isbn | 3-938616-40-7 | |
dc.identifier.uri | http://hdl.handle.net/11858/00-1735-0000-0001-3458-4 | |
dc.description.abstract | The measurement of the anisotropy of
the magnetic susceptibility (AMS) is now routinely used since more than four
decades in the analyses of rock fabrics in
granitic rocks (e.g. Stacy 1960, Henry
1975, Gleizes et al. 1993). Even though
the intensity of fabrics in granitoids is
often weakly developed the significance
of orientation and shape of crystals is
the same like in other deformed rock
types. By revealing the distribution of
fabrics in plutonic rocks one of the still
ongoing discussions in granite tectonics
may be addressed: How did those
sometimes voluminous batholiths were
inflated in the middle crust? We are presenting
magnetic fabric data on a series
of Devonian batholiths that intruded
the polyphase deformed metaclastites of
the Sierra de San Luis (32°100– 33°200 S
/ 65°150 – 66°200 W) in central Argentina.
Regional considerations on the
tectonic regime during the emplacement
of the batholiths are inferred from combined
field, microstructural and AMS
observations... | |
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 | VKA 200 | |
dc.subject.gok | TOT 320 | |
dc.subject.gok | VKB 111 | |
dc.subject.gok | VAC 200 | |
dc.subject.gok | VEX 200 | |
dc.subject.gok | TSX 000 | |
dc.title | Syn-kinematic magma ascent and batholith inflation (Sierra de San Luis/Argentina) | |
dc.type | anthologyArticle | |
dc.subject.gokverbal | Gefügekunde der Gesteine | |
dc.subject.gokverbal | Paläomagnetismus {Geophysik} | |
dc.subject.gokverbal | Granitische Gesteine {Petrologie} | |
dc.subject.gokverbal | Plutonismus {Geologie} | |
dc.subject.gokverbal | Argentinien {Geologie} | |
dc.subject.gokverbal | Südamerika {Geophysik} | |
dc.bibliographicCitation.firstPage | 216 | |
dc.bibliographicCitation.lastPage | 220 | |
dc.identifier.doi | 10.23689/fidgeo-1885 | |
dc.type.version | publishedVersion | |
dc.subject.free | Sierra de San Luis | |
dc.subject.free | Devon | |
dc.subject.free | Batholith | |
dc.subject.free | Gedüge <Gesteinskunde> | |
dc.subject.free | Magnetische Suszeptibilität | |
dc.relation.collection | Geologische Wissenschaften | |
dc.description.type | conference | |