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• W2800370422 abstract "The Calabria Arc presents the highest probability of occurrence of major earthquakes in the Italian peninsula. Several destructive historical earthquakes (i.e. 1638, 1659, 1783, 1905 and 1908) affected, in particular, the Catanzaro Trough and its neighbouring areas. These events have been tentatively related to the activity of NE-SW trending normal faults. Some of these earthquakes have been followed by tsunamis, which caused further damages along the Tyrrhenian coast. In this paper, we reconstruct the Quaternary evolution of the Catanzaro Trough by combining field geo-structural and marine geophysical data. The results have been compared with existing database of earthquake focal mechanisms, updated with 8 new focal solutions performed in the present work. Analysis of faults offsetting the Lower-Middle Pleistocene deposits shows that the Catanzaro Trough experienced transcurrent and extensional phases of deformation. In particular, conjugate systems with NW-SE right-lateral and NE-SW left lateral faults were observed to displace the Lower Pleistocene deposits. Whereas NE–SW and N-S oriented normal faults have been identified as the main fault systems acting during late Pleistocene-Holocene phase. The interpretation of on-land structural datasets has been supported by geophysical data (multichannel and Chirp profiles) acquired in the offshore and onshore of the study area. Multidisciplinary approach has allowed to define NE-SW elongated sedimentary basins, as the Lamezia Basin, bordered on the one hand by Sant’Eufemia Fault that may extend up to 30 km-length, on the other hand by two overstepping faults, Vibo Valentia and San Pietro Lametino Faults. These findings carry some relevant implications in terms of seismic hazard, as they suggest that the longer fault segment, the greater its energetic seismic event. Finally, these data fit perfectly with the observed late Pleistocene-Holocene WNW-ESE extensional stress regime derived from existing and new database of earthquake focal mechanisms. This is in agreement with the orientation of the most seismically active grabens of the Calabrian Arc (the Crati, the Mesima and the Gioia Tauro Basins). Amongst these structural lineaments, the NE-SW and N-S trending normal faults play surely a relevant role as part of recent seismotectonics processes controlling the Late Quaternary geodynamics of the central Calabrian Arc, representing the source of the main destructive earthquakes occurred in the region." @default.
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• W2800370422 date "2018-01-01" @default.
• W2800370422 modified "2023-10-18" @default.
• W2800370422 title "Quaternary Stress Field and Faulting in the Western Part of the Catanzaro Trough (Calabria, Southern Italy)" @default.
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• W2800370422 cites W1968978247 @default.
• W2800370422 cites W1974493245 @default.
• W2800370422 cites W1974727405 @default.
• W2800370422 cites W1975613234 @default.
• W2800370422 cites W1980918384 @default.
• W2800370422 cites W1994378451 @default.
• W2800370422 cites W1997465526 @default.
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• W2800370422 cites W2007951133 @default.
• W2800370422 cites W2012100668 @default.
• W2800370422 cites W2012376219 @default.
• W2800370422 cites W2016013984 @default.
• W2800370422 cites W2016384800 @default.
• W2800370422 cites W2018179376 @default.
• W2800370422 cites W2024109686 @default.
• W2800370422 cites W2035113065 @default.
• W2800370422 cites W2040616304 @default.
• W2800370422 cites W2046395789 @default.
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• W2800370422 cites W2054451772 @default.
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• W2800370422 cites W2077860566 @default.
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• W2800370422 doi "https://doi.org/10.1007/978-3-319-77359-9_28" @default.
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