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.

Feldspar deformation in greenschist facies shear zones (Aar-Massif, Switzerland)

Hauten, Sarah
Handy, Mark R.ORCIDiD
Dobmeier, Christoph
2006
Universitätsverlag Göttingen
Article in Anthology
Verlagsversion
Deutsch
11. Symposium "Tektonik, Struktur- und Kristallingeologie"
DOI: https://doi.org/10.23689/fidgeo-1848
Hauten, Sarah; Handy, Mark R.; Dobmeier, Christoph, 2006: Feldspar deformation in greenschist facies shear zones (Aar-Massif, Switzerland). In: Philipp, S.; Leiss, B; Vollbrecht, A.; Tanner, D.; Gudmundsson, A. (eds.): 11. Symposium "Tektonik, Struktur- und Kristallingeologie"; 2006, Univ.-Verl. Göttingen, p. 84 - 85., , DOI: 10.23689/fidgeo-1848.
 
Thumbnail
View/Open
Hauten-etal.pdf (133.2Kb)
Metadata Export:
Endnote
BibTex
RIS
  • Abstract
Granitic gneisses of the Central Aar Granite host a shear zone network that formed at greenschist facies conditions. The work area is located in the Bächlital (Grimsel area, Central Switzerland) and was chosen for the analysis of shear zones because of the weakly anisotropic fabric of the host gneisses. Contrary to previous publications (e.g. Choukroune & Gapais, 1983), none of these host rocks are undeformed. They contain a penetrative foliation (S1) that strikes consistently ENE-WSW with a steep dip of around 70° to the south. This foliation is overprinted by the aforementioned shear zone network, which was the main focus of this study...
Statistik:
View Statistics
Collection
  • 11. Symposium "Tektonik, Struktur- und Kristallingeologie" , 2006-03 [111]
Subjects:
Aarmassiv
Scherzone
Granitgneis
Feldspäte
Deformation <Geologie>
Gesteinsdeformation {Strukturgeologie}
Gefügekunde der Gesteine
Metamorphe Komplexe, Alpen {Petrologie}
Schweizer Alpen {Geologie}
Metamorphite aus sauren bis intermediären Edukten {Petrologie}
Produkte mechanischer Deformation {Petrologie}
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