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.

Measurement of calcite crystallographic-preferred orientations by magnetic anisotropy and comparison to diffraction methods

Schmidt, Volkmar
Hirt, Ann M.
Burlini, Luigi
Leiss, BerndORCIDiD
Walter, Jens M.ORCIDiD
2006
Universitätsverlag Göttingen
Article in Anthology
Verlagsversion
Deutsch
11. Symposium "Tektonik, Struktur- und Kristallingeologie"
DOI: https://doi.org/10.23689/fidgeo-1895
Schmidt, Volkmar; Hirt, Ann M.; Burlini, Luigi; Leiss, Bernd; Walter, Jens M., 2006: Measurement of calcite crystallographic-preferred orientations by magnetic anisotropy and comparison to diffraction methods. In: Philipp, S.; Leiss, B; Vollbrecht, A.; Tanner, D.; Gudmundsson, A. (eds.): 11. Symposium "Tektonik, Struktur- und Kristallingeologie"; 2006, Univ.-Verl. Göttingen, p. 194 - 195., , DOI: 10.23689/fidgeo-1895.
 
Thumbnail
View/Open
Schmidt-etal.pdf (533.8Kb)
Metadata Export:
Endnote
BibTex
RIS
  • Abstract
The anisotropy of magnetic susceptibility (AMS) of rocks reflects the preferred orientations of minerals. Therefore AMS is a quick and easy way to characterize rock fabrics (Hrouda 1982,Borradaile 1988); the obtained result is also called the magnetic fabric of the rock. The method has been often used to measure the orientation of ferromagnetic minerals, mainly magnetite, but in recent studies it has been increasingly used to measure textures of paramagnetic minerals as phyllosilicates (Lüneburg et al. 1999, Cifelli et al. 2004). A further application is the measurement of diamagnetic textures, especially calcite textures. Calcite is suitable for the AMS method, because it has a high magnetic anisotropy with the minimum susceptibility along the crystallographic c-axis. Therefore a preferred orientation of the c-axes, which can be induced by deformation, generates a magnetic fabric...
Statistik:
View Statistics
Collection
  • 11. Symposium "Tektonik, Struktur- und Kristallingeologie" , 2006-03 [111]
Subjects:
Calzit
Magnetische Suszeptibilität
Kristallorientierung
Röntgendiffraktometrie
Neutronendiffraktometrie
Vergleichsmessung
Gefügekunde der Gesteine
Methodik {Strukturgeologie}
Erdmagnetische Verfahren {Geophysik}
Gesteinsmagnetismus {Geophysik}
Röntgenanalyse {Mineralogie: Kristallographie}
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