Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/13645
Authors: Maesano, Francesco Emanuele* 
Volpi, Valentina* 
Civile, Dario* 
Basili, Roberto* 
Conti, Alessia* 
Tiberti, Mara Monica* 
Accettella, Daniela* 
Conte, Riccardo* 
Zgur, Fabrizo* 
Rossi, Giuliana* 
Title: Active Extension in a Foreland Trapped Between Two Contractional Chains: The South Apulia Fault System (SAFS)
Journal: Tectonics 
Series/Report no.: /39 (2020)
Publisher: Wiley
Issue Date: 11-Jun-2020
DOI: 10.1029/2020TC006116
URL: https://agupubs.onlinelibrary.wiley.com/doi/full/10.1029/2020TC006116
Keywords: active tectonics
apulia
south apulia fault system
1743 earthquake
marine geology
stable continental region
ionian sea
active faults
subsurface geology
seismic interpretation
Subject Classification04.04. Geology 
04.07. Tectonophysics 
04.02. Exploration geophysics 
Abstract: The response of continental forelands to subduction and collision is a widely investigated topic in geodynamics. The deformation occurring within a foreland shared by two opposite‐verging chains, however, is uncommon and poorly understood. The Apulia Swell in the southern end of the Adria microplate (Africa‐Europe plate boundary, central Mediterranean Sea) represents one of these cases, as it is the common foreland of the SW verging Albanides‐Hellenides and the NE verging Southern Apennines merging into the SSE verging Calabrian Arc. We investigated the internal deformation of the Apulia Swell using multiscale geophysical data: multichannel seismic profiles recording up to 12‐s two‐way time (TWT) for a consistent image of the upper crust; high‐resolution multichannel seismic profiles, high‐resolution multibeam bathymetry, and CHIRP profiles acquired by R/V OGS Explora to constrain the Quaternary geological record. The results of our analyses characterize the geometry of the South Apulia Fault System (SAFS), a 100‐km‐long and 12‐km‐wide structure attesting an extensional (and possibly transtensional) response of the foreland to the two contractional fronts. The SAFS consists of two NW‐SE right‐stepping master faults and several secondary structures. The SAFS activity spans from the Early Pleistocene through the Holocene, as testified by the bathymetric and high‐resolution seismic data, with long‐term slip rates in the range of 0.2–0.4 mm/yr. Considering the position within an area with few or none other active faults in the surroundings, the dimension, and the activity rates, the SAFS can be a candidate causative fault of the 20 February 1743, M 6.7, earthquake.
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