Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
8908826 | Tectonophysics | 2018 | 41 Pages |
Abstract
We ascribe the slip change along the Sciacca Fault, from a right-lateral transcurrent regime to the present-day left-lateral kinematics to a change of principal horizontal stress direction starting from Late Pliocene.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth-Surface Processes
Authors
Jakub Fedorik, Giovanni Toscani, Emanuele Lodolo, Dario Civile, Lorenzo Bonini, Silvio Seno,