Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
8907740 | Journal of South American Earth Sciences | 2018 | 22 Pages |
Abstract
The data shown here, let characterized the Incachule district as a shallow low sulfidation epithermal system hosted in a collapse caldera. Our data also indicate that mineralization is structurally controlled by a fault system related to the 10.3 Ma collapse of Aguas Calientes caldera. The interpreted local stress field is consistent with the regional one.
Keywords
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth and Planetary Sciences (General)
Authors
Natalia Salado Paz, Iván Petrinovic, Margarita Do Campo, José Affonso Brod, Fernando Nieto, Valmir da Silva Souza, Klauss Wemmer, Patricio Payrola, Roberto Ventura,