Articles | Volume 9, issue 2
https://doi.org/10.5194/se-9-469-2018
https://doi.org/10.5194/se-9-469-2018
Research article
 | 
23 Apr 2018
Research article |  | 23 Apr 2018

Controls on fault zone structure and brittle fracturing in the foliated hanging wall of the Alpine Fault

Jack N. Williams, Virginia G. Toy, Cécile Massiot, David D. McNamara, Steven A. F. Smith, and Steven Mills

Viewed

Total article views: 3,620 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
2,210 1,221 189 3,620 606 152 160
  • HTML: 2,210
  • PDF: 1,221
  • XML: 189
  • Total: 3,620
  • Supplement: 606
  • BibTeX: 152
  • EndNote: 160
Views and downloads (calculated since 10 Oct 2017)
Cumulative views and downloads (calculated since 10 Oct 2017)

Viewed (geographical distribution)

Total article views: 3,620 (including HTML, PDF, and XML) Thereof 3,261 with geography defined and 359 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Discussed (final revised paper)

Discussed (preprint)

Latest update: 03 Nov 2024
Download
Short summary
We present new data on the orientation of fractures, their fill, and their density around the Alpine Fault, a plate boundary fault on the South Island of New Zealand. Fractures < 160 m of the fault are filled and show a range of orientations, whilst fractures at greater distances (< 500 m) are open and parallel to the rock's mechanical weakness. We interpret the latter fracture set to reflect near-surface processes, whilst the latter are potentially linked to deep-seated Alpine Fault seismicity.