Articles | Volume 11, issue 6
https://doi.org/10.5194/se-11-2015-2020
https://doi.org/10.5194/se-11-2015-2020
Research article
 | 
09 Nov 2020
Research article |  | 09 Nov 2020

Using horizontal-to-vertical spectral ratios to construct shear-wave velocity profiles

Janneke van Ginkel, Elmer Ruigrok, and Rien Herber

Viewed

Total article views: 2,047 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,240 728 79 2,047 142 80 65
  • HTML: 1,240
  • PDF: 728
  • XML: 79
  • Total: 2,047
  • Supplement: 142
  • BibTeX: 80
  • EndNote: 65
Views and downloads (calculated since 09 Jun 2020)
Cumulative views and downloads (calculated since 09 Jun 2020)

Viewed (geographical distribution)

Total article views: 2,047 (including HTML, PDF, and XML) Thereof 1,815 with geography defined and 232 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 22 Apr 2024
Download
Short summary
Knowledge of subsurface velocities is key to understand how earthquake waves travel through the Earth. We present a method to construct velocity profiles for the upper sediment layer on top of the Groningen field, the Netherlands. Here, the soft-sediment layer causes resonance of seismic waves, and this resonance is used to compute velocities from. Recordings from large earthquakes and the background noise signals are used to derive reliable velocities for the deep sedimentary layer.