Articles | Volume 2
https://doi.org/10.5194/sand-2-69-2023
https://doi.org/10.5194/sand-2-69-2023
Conference Abstract
 | 
06 Sep 2023
Conference Abstract |  | 06 Sep 2023

The anisotropy of geomaterial granite

Franz Müller, Peter Hallas, and Uwe Kroner

Viewed

Total article views: 473 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
341 113 19 473 66 36 86
  • HTML: 341
  • PDF: 113
  • XML: 19
  • Total: 473
  • Supplement: 66
  • BibTeX: 36
  • EndNote: 86
Views and downloads (calculated since 06 Sep 2023)
Cumulative views and downloads (calculated since 06 Sep 2023)
Latest update: 02 Dec 2025
Download
Short summary
Granites appear to be isotropic, which qualifies them as suitable crystalline host rocks for nuclear waste repository sites. However, despite their optical appearance, granites show a primary structural anisotropy (Bouchez, 1997) that evolved during emplacement and crystallization of the melt. We present the first results of a systematic study of felsic plutonites, i.e. the GAME project, which aims to lead to a better understanding of felsic plutonites as a geomaterial.
Share