Aeromagnetic investigation of southern Calabria and the Messina Straits (Italy): Tracking seismogenic sources of 1783 and 1908 earthquakes

Southern Calabria and the NE corner of Sicily (Italy) were struck in 1783 and 1908 A.D. by two of
the most catastrophic earthquakes ever in European history. Although it is generally acknowledged that the
seisms were yielded by normal faults rupturing the upper crust of the Calabria-Peloritani terrane, no consensus
exists on seismogenic source location and orientation. Here we report on a high-resolution low-altitude
aeromagnetic survey of southern Calabria and Messina Straits. In southern Calabria we document a broad
weakly positive (5–10 nT) anomaly zone interrupted by three en echelon SW-NE null to negative magnetic
anomaly corridors. Euler deconvolution and magneticmodeling show that the anomaly pattern is produced by
a 1–1.5 km thick crustal “layer” located within 3km depth. This layer is offset by a 25km long NE trending fault
that corresponds to the Armo normal fault, recently inferred to be the source for the 1908 earthquake. Few
kilometers to the south, we also document a subparallel and previously unrecognized fault, entering the
Messina Straits and likely joining the Armo fault at depth. Further east, we model a 40 km long normal fault,
probably extending northeastward for additional 40 km, running along the south Calabria axis from
Aspromonte to the Serre mountains and partly following the 18 km long surface rupture witnessed by
Déodat de Dolomieu after the 1783 earthquake. Thus, aeromagnetic data suggest that the sources of the
1783 and 1908 earthquakes are en echelon faults belonging to the same NW dipping normal fault system
straddling the whole southern Calabria.