Zur Kurzanzeige

dc.contributor.authorSteenken, André
dc.contributor.authorSiegesmund, Siegfried
dc.contributor.authorLuchi, Mónica G. López de
dc.contributor.authorRapalini, Augusto
dc.contributor.authorWemmer, Klaus
dc.contributor.editorPhilipp, Sonja
dc.contributor.editorLeiss, Bernd
dc.contributor.editorVollbrecht, Axel
dc.contributor.editorTanner, David
dc.contributor.editorGudmundsson, Agust
dc.date.accessioned2010-11-26T13:21:25Z
dc.date.accessioned2013-01-28T10:20:22Z
dc.date.available2010-11-26T13:21:25Z
dc.date.available2013-01-28T10:20:22Z
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. 216 - 220.
dc.identifier.isbn3-938616-40-7
dc.identifier.urihttp://hdl.handle.net/11858/00-1735-0000-0001-3458-4
dc.description.abstractThe 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.mimetypeapplication/pdf
dc.language.isodeu
dc.publisherUniversitätsverlag Göttingen
dc.relation.ispartof11. Symposium "Tektonik, Struktur- und Kristallingeologie"
dc.subject.ddc551
dc.subject.gokVKA 200
dc.subject.gokTOT 320
dc.subject.gokVKB 111
dc.subject.gokVAC 200
dc.subject.gokVEX 200
dc.subject.gokTSX 000
dc.titleSyn-kinematic magma ascent and batholith inflation (Sierra de San Luis/Argentina)
dc.typeanthologyArticle
dc.subject.gokverbalGefügekunde der Gesteine
dc.subject.gokverbalPaläomagnetismus {Geophysik}
dc.subject.gokverbalGranitische Gesteine {Petrologie}
dc.subject.gokverbalPlutonismus {Geologie}
dc.subject.gokverbalArgentinien {Geologie}
dc.subject.gokverbalSüdamerika {Geophysik}
dc.bibliographicCitation.firstPage216
dc.bibliographicCitation.lastPage220
dc.identifier.doi10.23689/fidgeo-1885
dc.type.versionpublishedVersion
dc.subject.freeSierra de San Luis
dc.subject.freeDevon
dc.subject.freeBatholith
dc.subject.freeGedüge <Gesteinskunde>
dc.subject.freeMagnetische Suszeptibilität
dc.relation.collectionGeologische Wissenschaften
dc.description.typeconference


Dateien zu dieser Ressource

Thumbnail

Das Dokument erscheint in:

Zur Kurzanzeige