Articles | Volume 18, issue 2
https://doi.org/10.5194/nhess-18-531-2018
https://doi.org/10.5194/nhess-18-531-2018
Research article
 | 
21 Feb 2018
Research article |  | 21 Feb 2018

Implications from palaeoseismological investigations at the Markgrafneusiedl Fault (Vienna Basin, Austria) for seismic hazard assessment

Esther Hintersberger, Kurt Decker, Johanna Lomax, and Christopher Lüthgens

Viewed

Total article views: 3,712 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
2,282 1,239 191 3,712 460 128 154
  • HTML: 2,282
  • PDF: 1,239
  • XML: 191
  • Total: 3,712
  • Supplement: 460
  • BibTeX: 128
  • EndNote: 154
Views and downloads (calculated since 15 May 2017)
Cumulative views and downloads (calculated since 15 May 2017)

Viewed (geographical distribution)

Total article views: 3,712 (including HTML, PDF, and XML) Thereof 3,574 with geography defined and 138 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 13 Aug 2025
Download
Short summary
The Vienna Basin is a low seismicity area, where historical data do not identify all potential earthquake sources. Despite observed Quaternary offset, there are no earthquakes along the Markgrafneusiedl Fault (MF). Results from 3 palaeoseismic trenches show evidence for 5–6 earthquakes with magnitudes up to M = 6.8 during the last 120 kyr. Therefore the MF should be considered as a seismic source, together with similar faults in the Vienna Basin, increasing the seismic potential close to Vienna.
Share
Altmetrics
Final-revised paper
Preprint