Articles | Volume 9, issue 3
https://doi.org/10.5194/se-9-683-2018
https://doi.org/10.5194/se-9-683-2018
Research article
 | 
29 May 2018
Research article |  | 29 May 2018

Permeability and seismic velocity anisotropy across a ductile–brittle fault zone in crystalline rock

Quinn C. Wenning, Claudio Madonna, Antoine de Haller, and Jean-Pierre Burg

Viewed

Total article views: 3,295 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
1,858 1,282 155 3,295 129 121
  • HTML: 1,858
  • PDF: 1,282
  • XML: 155
  • Total: 3,295
  • BibTeX: 129
  • EndNote: 121
Views and downloads (calculated since 05 Mar 2018)
Cumulative views and downloads (calculated since 05 Mar 2018)

Viewed (geographical distribution)

Total article views: 3,295 (including HTML, PDF, and XML) Thereof 2,989 with geography defined and 306 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Discussed (final revised paper)

Latest update: 18 Mar 2024
Download
Short summary
We measured the elastic and fluid flow properties in a ductile-brittle shear zone. The results suggest that although brittle deformation has persisted in the recent fault evolution, precursory ductile microstructure continues to control the petrophysical properties outside the fault core. The results are a glimpse into the evolutionary path of a shear zone during the ductile to brittle transition and are insightful for geothermal energy and geologic waste disposal exploitation and usage.