Structural complexities and tectonic barriers controlling recent seismic activity of the Pollino area (Calabria-Lucania, Southern Italy) -constraints from stress inversion and 3D fault model building



Figure 1 :

 1 Figure 1: (a) location map with temporary and permanent seismic stations (black used for 




  map showing the main faults mapped on a 10 m-resolution DEM (Tarquini 23 et al., 2012). The structural sites are divided into black circles if used for the pseudo-focal mechanisms reported in Figure 3 of 24 the main text, and white circles. BAT= Battendiero fault; GCG= Gada-Ciagola fault; PPS= Papasidero fault; AVN= Avena 25 fault; VCT= Fosso della Valle-Campotenese fault; RSB= Rotonda-Sambucoso; CVN= Cozzo Vardo-Cozzo Nisco fault; 26 MPR= Morano Calabro-Piano di Ruggio fault; VPP= Viggianello -Piano di Pollino fault; GDN= Gaudolino fault; POL= 27 Pollino fault; CAS= Castrovillari fault; SDD= Serra Dolcedorme fault; PAC= Monte Palanuda -Campolungo fault; CPST= 28 Castello Seluci-Piana Perretti fault. 




  


Table 1 :

 1 Summary table of the seismogenic boxes' parameters. 


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Daniele Cirillo, Cristina Totaro, Giusy Lavecchia, Barbara Orecchio, Rita De Nardis, Debora Presti, Federica Ferrarini, Simone Bello, Francesco Brozzetti
Structural complexities and tectonic barriers controlling recent seismic activity of the Pollino area (Calabria-Lucania, Southern Italy) -constraints from stress inversion and 3D fault model building