dc.contributor.author | Nüchter, Jens-Alexander | |
dc.contributor.author | Stöckhert, Bernhard | |
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 | 2010-11-26T13:21:09Z | |
dc.date.accessioned | 2013-01-28T10:19:54Z | |
dc.date.available | 2010-11-26T13:21:09Z | |
dc.date.available | 2013-01-28T10:19:54Z | |
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. 155 - 156. | |
dc.identifier.isbn | 3-938616-40-7 | |
dc.identifier.uri | http://hdl.handle.net/11858/00-1735-0000-0001-341D-8 | |
dc.description.abstract | Metamorphic rocks approaching the
crustal scale brittle-ductile transition
(BDT) during exhumation are expected
to become increasingly affected by short
term stress fluctuations related to seismic
activity in the overlying seismogenic
layer (schizosphere), while still residing
in a long-term viscous environment
(plastosphere). The structural and microstructural
record of quartz veins in
low grade – high pressure metamorphic
rocks from southern Evia, Greece, yields
insight into the processes and conditions
just beneath the long-term BDT at temperatures
of about 300 to 350°C, with
switches between brittle failure and viscous
flow as a function of imposed stress
or strain rate... | |
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 | VAE 400 | |
dc.subject.gok | VAE 150 | |
dc.subject.gok | VKB 130 | |
dc.subject.gok | VEF 300 | |
dc.title | Fracturing and vein formation in the middle crust - a record of co-seismic loading and post-seismic stress relaxation | |
dc.type | anthologyArticle | |
dc.subject.gokverbal | Tektogenese {Geologie} | |
dc.subject.gokverbal | Strukturelle Erscheinungen {Strukturgeologie} | |
dc.subject.gokverbal | Petrologie der Ganggesteine | |
dc.subject.gokverbal | Griechenland und griechische Inseln {Geologie} | |
dc.bibliographicCitation.firstPage | 155 | |
dc.bibliographicCitation.lastPage | 156 | |
dc.identifier.doi | 10.23689/fidgeo-1852 | |
dc.type.version | publishedVersion | |
dc.subject.free | Euböa | |
dc.subject.free | Krustenbewegung | |
dc.subject.free | Hydraulische Rissbildung | |
dc.subject.free | Bruch <Geologie> | |
dc.subject.free | Quarzgang | |
dc.relation.collection | Geologische Wissenschaften | |
dc.description.type | conference | |