Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/14248
Authors: Totaro, Cristina* 
Seeber, L.* 
Waldhauser, F.* 
Steckler, M.* 
Gervasi, Anna* 
Guerra, Ignazio* 
Orecchio, Barbara* 
Presti, D.* 
Title: An Intense Earthquake Swarm in the Southernmost Apennines: Fault Architecture from High-Resolution Hypocenters and Focal Mechanisms
Journal: Bulletin of the Seismological Society of America 
Series/Report no.: 6/105 (2015)
Publisher: SSA
Issue Date: 2015
DOI: 10.1785/0120150074
URL: https://pubs.geoscienceworld.org/ssa/bssa/article-abstract/105/6/3121/332020/An-Intense-Earthquake-Swarm-in-the-Southernmost?redirectedFrom=fulltext
Abstract: Between 2010 and 2013, the Pollino Mountains region (south Italy), already proposed as a seismic gap, was affected by a seismic crisis of more than 5000 small-to-moderate earthquakes (maximum magnitude ML 5.0). Preliminary analyses performed in a previous work highlighted that this activity can be ascribed to normal faulting on north-northwest-trending west-dipping dislocation surfaces consistent with the general seismotectonic frame of the southern Apennines. This work contributes additional data and a more sophisticated analyses that highlight new features of the seismic swarm and support a new interpretation for the study area. We obtained high-precision locations and focal mechanisms using the double-difference method and the cut-and-paste waveform inversion method, respectively. The 3D patterns of hypocenters and focal mechanisms consistently image an ∼10-km-long north-northwest-striking and west-dipping fault zone between 5 and 10 km depth, with predominantly extensional kinematics. The high-resolution data show that this zone broadens from north to south as a result of secondary faulting. The depicted geometry, with preliminary geological observation, leads to the hypothesis of multiple seismogenic normal faults rooted into more regional shallow-dipping detachments inherited from the pre-existing Apennine thrust tectonics.
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