Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
5781544 | Tectonophysics | 2017 | 65 Pages |
Abstract
We find a few right-lateral strike-slip focal mechanisms that possibly identify the prolongation of the strike-slip kinematics in the Gargano-Apulia foreland to the west, and mark the passage to the NW-SE striking normal faults of the inner Apenninic belt. The seismicity and stress distribution we observe might be consistent with a fragmented tectonic scenario in which faults with small dimensions release seismic energy in a diffused way.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth-Surface Processes
Authors
A. Frepoli, G.B. Cimini, P. De Gori, G. De Luca, A. Marchetti, S. Monna, C. Montuori, N.M. Pagliuca,