Articles | Volume 8, issue 5
https://doi.org/10.5194/se-8-1071-2017
https://doi.org/10.5194/se-8-1071-2017
Research article
 | 
17 Oct 2017
Research article |  | 17 Oct 2017

The grain size(s) of Black Hills Quartzite deformed in the dislocation creep regime

Renée Heilbronner and Rüdiger Kilian

Viewed

Total article views: 3,469 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
2,010 1,295 164 3,469 314 147 194
  • HTML: 2,010
  • PDF: 1,295
  • XML: 164
  • Total: 3,469
  • Supplement: 314
  • BibTeX: 147
  • EndNote: 194
Views and downloads (calculated since 20 Mar 2017)
Cumulative views and downloads (calculated since 20 Mar 2017)

Viewed (geographical distribution)

Total article views: 3,469 (including HTML, PDF, and XML) Thereof 3,180 with geography defined and 289 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Discussed (final revised paper)

Discussed (preprint)

Latest update: 26 Jul 2024
Short summary
The crystallographic texture of experimentally sheared samples of dynamically recrystallized quartzite have been reanalyzed using EBSD. Detailed grain size analysis reveals that the recrystallized grain size depends not only on stress, as assumed in the recrystallized quartz piezometer of Stipp and Tullis (2003), but also on texture, grain-scale deformation intensity, and the kinematic framework of axial versus general shear experiments.