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dc.contributor.authorNeubert, Jana
dc.contributor.authorKlauw, Sebastiaan van der
dc.contributor.authorKley, Jonas
dc.contributor.editorPhilipp, Sonja
dc.contributor.editorLeiss, Bernd
dc.contributor.editorVollbrecht, Axel
dc.contributor.editorTanner, David
dc.contributor.editorGudmundsson, Agust
dc.date.accessioned2010-11-26T13:21:09Z
dc.date.accessioned2013-01-28T10:19:33Z
dc.date.available2010-11-26T13:21:09Z
dc.date.available2013-01-28T10:19:33Z
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. 146 - 151.
dc.identifier.isbn3-938616-40-7
dc.identifier.urihttp://hdl.handle.net/11858/00-1735-0000-0001-341F-4
dc.description.abstractThe research area is located in the Ruhla-Brotterode crystalline complex in the western part of the Thuringian Forest (Germany), about 20km southsouthwest of Eisenach. The investigated outcrops occur at the eastern and western flanks of the valleys north of the villages Trusetal and Hohleborn. Deformed magmatic veins only occur in the Hohleborn area. Both areas have relative fresh outcropping rocks, due to the steep relief, former quarries and fresh road cuts. According to Obst & Katzung (2000) several periods with the formation of magmatic veins with different chemical composition occur in the Ruhla-Brotterode crystalline complex. Presumably older lamprophyric veins and younger doleritic, syenitporphyric and granitporphyric veins have been identified (Obst & Katzung 2000). Benek & Schust (1988) already pointed out that some of these magmatic veins have experienced ductile deformation. The subject of this work is the occurrence of deformed magmatic veins in the Hohleborn area. The contact to their host rocks, their petrography and their microfabrics have been investigated and related to deformation processes, which led to a better understanding of their deformation conditions within the late-to post-variscan development of the area.
dc.format.mimetypeapplication/pdf
dc.language.isodeu
dc.publisherUniversitätsverlag Göttingen
dc.relation.ispartof11. Symposium "Tektonik, Struktur- und Kristallingeologie"
dc.subject.ddc551
dc.subject.gokVKB 290
dc.subject.gokVEB 125
dc.subject.gokVAE 140
dc.subject.gokVKA 200
dc.titleMicrofabrics and deformation processes in magmatic veins of the Thuringian Forest, Germany
dc.typeanthologyArticle
dc.subject.gokverbalMetamorphe Komplexe, Mitteleuropa {Petrologie}
dc.subject.gokverbalHessisch-thüringisches Bergland {Geologie}
dc.subject.gokverbalGesteinsdeformation {Strukturgeologie}
dc.subject.gokverbalGefügekunde der Gesteine
dc.bibliographicCitation.firstPage146
dc.bibliographicCitation.lastPage151
dc.identifier.doi10.23689/fidgeo-1828
dc.type.versionpublishedVersion
dc.subject.freeRhulaer Kristallin
dc.subject.freeGanggestein
dc.subject.freeDeformation <Geologie>
dc.subject.freeMikrostruktur
dc.relation.collectionGeologische Wissenschaften
dc.description.typeconference


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