Articles | Volume 25, issue 1
https://doi.org/10.5194/npg-25-251-2018
https://doi.org/10.5194/npg-25-251-2018
Research article
 | 
29 Mar 2018
Research article |  | 29 Mar 2018

Complex interplay between stress perturbations and viscoelastic relaxation in a two-asperity fault model

Emanuele Lorenzano and Michele Dragoni

Viewed

Total article views: 2,275 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
1,388 746 141 2,275 123 133
  • HTML: 1,388
  • PDF: 746
  • XML: 141
  • Total: 2,275
  • BibTeX: 123
  • EndNote: 133
Views and downloads (calculated since 26 Oct 2017)
Cumulative views and downloads (calculated since 26 Oct 2017)

Viewed (geographical distribution)

Total article views: 2,275 (including HTML, PDF, and XML) Thereof 2,128 with geography defined and 147 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 23 Nov 2024
Download
Short summary
We devise a model to investigate the interplay between two common phenomena affecting the evolution of a seismogenic fault: the occurrence of earthquakes on neighbouring faults and the partial degree of anelasticity of rocks in the upper mantle, a feature that is often manifested by a post-seismic process known as viscoelastic relaxation. We show how this process dramatically complicates the way an earthquake may alter the magnitude and timing of a seismic event on the perturbed fault.