Articles | Volume 12, issue 1
https://doi.org/10.5194/se-12-253-2021
https://doi.org/10.5194/se-12-253-2021
Research article
 | 
29 Jan 2021
Research article |  | 29 Jan 2021

The Piuquencillo fault system: a long-lived, Andean-transverse fault system and its relationship with magmatic and hydrothermal activity

José Piquer, Orlando Rivera, Gonzalo Yáñez, and Nicolás Oyarzún

Viewed

Total article views: 2,111 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,405 663 43 2,111 136 30 32
  • HTML: 1,405
  • PDF: 663
  • XML: 43
  • Total: 2,111
  • Supplement: 136
  • BibTeX: 30
  • EndNote: 32
Views and downloads (calculated since 21 Aug 2020)
Cumulative views and downloads (calculated since 21 Aug 2020)

Viewed (geographical distribution)

Total article views: 2,111 (including HTML, PDF, and XML) Thereof 1,953 with geography defined and 158 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 24 Apr 2024
Download
Short summary
A proper recognition of deep, long-lived fault systems is very important for society. They can produce potentially dangerous earthquakes. They can also act as pathways for magmas and hydrothermal fluids, leading to the formation of volcanoes, geothermal systems and mineral deposits. However, the manifestations of these very old faults in the present-day surface can be very subtle. Here, we present a detailed, multi-disciplinary study of a fault system of this type in the Andes of central Chile.