| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 9527074 | Tectonophysics | 2005 | 18 Pages |
Abstract
We interpret that destabilization of sediments occurs most probably in response to local reactivation of faults within the Mejillones peninsula during strong earthquakes, especially the Mejillones fault.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth-Surface Processes
Authors
Gabriel Vargas, Luc Ortlieb, Emmanuel Chapron, Jorge Valdes, Carlos Marquardt,