Active tectonics along the Nebrodi–Peloritani boundary in northeastern Sicily (Southern Italy)

2015 ◽  
Vol 659 ◽  
pp. 1-11 ◽  
Author(s):  
F. Pavano ◽  
G. Romagnoli ◽  
G. Tortorici ◽  
S. Catalano
Lithosphere ◽  
2016 ◽  
Vol 8 (6) ◽  
pp. 633-648 ◽  
Author(s):  
Francesco Pavano ◽  
Frank J. Pazzaglia ◽  
Stefano Catalano

2005 ◽  
Vol 162 (4) ◽  
pp. 715-727
Author(s):  
Domenica Termini ◽  
Antonio Teramo ◽  
Carla Bottari

2021 ◽  
Vol 11 (16) ◽  
pp. 7512
Author(s):  
Marilena Filippucci ◽  
Salvatore Lucente ◽  
Edoardo Del Pezzo ◽  
Salvatore de Lorenzo ◽  
Giacomo Prosser ◽  
...  

We investigate crustal seismic attenuation by the coda quality parameter (Qc) in the Gargano area (Southern Italy), using a recently released dataset composed of 191 small earthquakes (1.0 ≤ ML ≤ 2.8) recorded by the local OTRIONS and the Italian INGV seismic networks, over three years of seismic monitoring. Following the single back-scattering theoretical assumption, Qc was computed using different frequencies (in the range of 2–16 Hz) and different lapse times (from 10 to 40 s). The trend of Qc vs. frequency is the same as that observed in the adjacent Umbria-Marche region. Qc at 1 Hz varies between 11 and 63, indicating that the area is characterized by active tectonics, despite the absence of high-magnitude earthquakes in recent decades. The 3D mapping procedure, based on sensitivity kernels, revealed that the Gargano Promontory is characterized by very low and homogeneous Qc at low frequencies, and by high and heterogeneous Qc at high frequencies. The lateral variations of Qc at 12 Hz follow the trend of the Moho in this region and are in good agreement with other geophysical observations.


1995 ◽  
Vol 243 (1-2) ◽  
pp. 37-55 ◽  
Author(s):  
Luigi Tortorici ◽  
Carmelo Monaco ◽  
Carlo Tansi ◽  
Ornella Cocina

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