Articles | Volume 24, issue 3
https://doi.org/10.5194/npg-24-419-2017
https://doi.org/10.5194/npg-24-419-2017
Research article
 | 
04 Aug 2017
Research article |  | 04 Aug 2017

An upper limit for slow-earthquake zones: self-oscillatory behavior through the Hopf bifurcation mechanism from a spring-block model under lubricated surfaces

Valentina Castellanos-Rodríguez, Eric Campos-Cantón, Rafael Barboza-Gudiño, and Ricardo Femat

Viewed

Total article views: 2,268 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,250 813 205 2,268 283 153 195
  • HTML: 1,250
  • PDF: 813
  • XML: 205
  • Total: 2,268
  • Supplement: 283
  • BibTeX: 153
  • EndNote: 195
Views and downloads (calculated since 14 Nov 2016)
Cumulative views and downloads (calculated since 14 Nov 2016)

Viewed (geographical distribution)

Total article views: 2,268 (including HTML, PDF, and XML) Thereof 2,195 with geography defined and 73 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 14 Jun 2024
Download
Short summary
A spring-block model is used to determine an upper limit of slow-earthquake zones through study of self-oscillatory behavior with the Hopf bifurcation mechanism. What is the role of fluids in the mechanism of energy dissipation? Are the variations in oscillatory behavior (in the transition zone) due to external forces? What are the limits of parameters for this to occur? The proposed limit makes a difference to oscillatory behavior. Oscillation frequency, L, and fluids are related to results.