Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
8908773 | Tectonophysics | 2018 | 41 Pages |
Abstract
Our results depict a clear seismic signature of the Victoria Lines Fault, characterized by low seismic velocity and high amplification of ground motion. We hypothesize that, during the Middle Pleistocene, faulting may have affected the basal part of the red beds, so that this part of the investigated complex fault-system may be considered inactive since ~0.6â¯Myr ago.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth-Surface Processes
Authors
Fabio Villani, Sebastiano D'Amico, Francesco Panzera, Maurizio Vassallo, George Bozionelos, Daniela Farrugia, Pauline Galea,