GEO-LEOedocs LogoGEO-LEOedocs Logo
  • GEO-LEO
    • Deutsch
    • English
  • GEO-LEO
  • English 
    • Deutsch
    • English
  • Login
View Item 
  •   Home
  • Alle Publikationen
  • Konferenzen
  • 11. Symposium "Tektonik, Struktur- und Kristallingeologie" , 2006-03
  • View Item
  •   Home
  • Alle Publikationen
  • Konferenzen
  • 11. Symposium "Tektonik, Struktur- und Kristallingeologie" , 2006-03
  • View Item
JavaScript is disabled for your browser. Some features of this site may not work without it.

Effect of crystallography and temperature on the development of quartz high-angle grain boundaries in metamorphic rocks

Liebl, Christoph
Kuntcheva, Boriana
Kruhl, Jörn H.ORCIDiD
Kunze, Karsten
2006
Universitätsverlag Göttingen
Article in Anthology
Verlagsversion
Deutsch
11. Symposium "Tektonik, Struktur- und Kristallingeologie"
DOI: https://doi.org/10.23689/fidgeo-1878
Liebl, Christoph; Kuntcheva, Boriana; Kruhl, Jörn H.; Kunze, Karsten, 2006: Effect of crystallography and temperature on the development of quartz high-angle grain boundaries in metamorphic rocks. In: Philipp, S.; Leiss, B; Vollbrecht, A.; Tanner, D.; Gudmundsson, A. (eds): 11. Symposium "Tektonik, Struktur- und Kristallingeologie"; 2006, Univ.-Verl. Göttingen, p. 132-134., , DOI: 10.23689/fidgeo-1878.
 
Thumbnail
View/Open
Liebl-etal.pdf (852.8Kb)
Metadata Export:
Endnote
BibTex
RIS
  • Abstract
Grain boundary migration during dynamic recrystallization of quartz results in grain boundary suturing of various extent. The geometry of the sutured boundaries is affected not only by temperature, strain rate, finite strain and differential stress, but also by internal properties such as the defect distribution and crystallographic orientations. Consequently, the grain boundary geometry may provide information about these conditions and properties. In continuation of a previous study (Kuntcheva et al.) the complete crystallographic orientation of quartz grain boundaries was measured, based on a combination of electron backscatter diffraction (EBSD) and universal-stage (U-stage) measurements. For this purpose a sample of granite from the northern Aar Massif (Central Alps, Switzerland) was taken, deformed at temperatures up to 300–350°C at the end of the Lepontine event of the Alpine Orogenesis...
Statistik:
View Statistics
Collection
  • 11. Symposium "Tektonik, Struktur- und Kristallingeologie" , 2006-03 [111]
Subjects:
Aare-Massiv
Granitgneis
Quarz
Rekristallisationstextur
Gefügekunde der Gesteine
Methodik {Strukturgeologie}
Geomechanik
GEO-LEO e-docs Lizenz

ImpressumPrivacy (Opt-Out)Cookie ConsentsAbout us/ContactDeposit LicenseSubmission hintsSupport: fid-geo-digi@sub.uni-goettingen.de
DFGSUBFID GEOFID Montan
 

 

Submit here
Submission hints
Search hints

All of Geo-Leo e-docsCommunities & CollectionsBy Issue DateContributorsSubjectsPeriodicalsTitlesThis CollectionBy Issue DateContributorsSubjectsPeriodicalsTitles

Statistics

View Usage Statistics

ImpressumPrivacy (Opt-Out)Cookie ConsentsAbout us/ContactDeposit LicenseSubmission hintsSupport: fid-geo-digi@sub.uni-goettingen.de
DFGSUBFID GEOFID Montan