Articles | Volume 13, issue 8
https://doi.org/10.5194/se-13-1169-2022
https://doi.org/10.5194/se-13-1169-2022
Research article
 | 
01 Aug 2022
Research article |  | 01 Aug 2022

Tectonic evolution of the Indio Hills segment of the San Andreas fault in southern California, southwestern USA

Jean-Baptiste P. Koehl, Steffen G. Bergh, and Arthur G. Sylvester

Viewed

Total article views: 1,990 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,376 556 58 1,990 179 34 34
  • HTML: 1,376
  • PDF: 556
  • XML: 58
  • Total: 1,990
  • Supplement: 179
  • BibTeX: 34
  • EndNote: 34
Views and downloads (calculated since 02 Feb 2022)
Cumulative views and downloads (calculated since 02 Feb 2022)

Viewed (geographical distribution)

Total article views: 1,990 (including HTML, PDF, and XML) Thereof 1,893 with geography defined and 97 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 25 Apr 2024
Download
Short summary
The San Andreas fault is a major active fault associated with ongoing earthquake sequences in southern California. The present study investigates the development of the Indio Hills area in the Coachella Valley along the main San Andreas fault and the Indio Hills fault. The Indio Hills area is located near an area with high ongoing earthquake activity (Brawley seismic zone), and, therefore, its recent tectonic evolution has implications for earthquake prediction.