SKS‐wave birefringence is likely caused by ongoing and/or fossil mantle flow. Splitting
parameters in the southern Tyrrhenian subduction zone define a quite complex pattern of fast …

The AlpArray programme is a multinational, European consortium to advance our understanding
of orogenesis and its relationship to mantle dynamics, plate reorganizations, surface …

We describe a set of seismological observations of the foreshock sequence preceding the 6
April 2009 M w 6.3 L'Aquila earthquake. The dense configuration of the seismic network in …

We compare microtremor data to weak-motion S-wave and coda recordings at sites in San
Francisco in order to clarify the range of applicability of microtremor data to ground-motion …

Combining tectonics, with seismological and geochemical data, we reconstruct the deformation
history of the presently narrow Calabrian slab and the path of mantle circulation during …

On May 20, 2012 (02:03:53 UTC), an Mw 5.86 (Ml 5.9) earthquake struck the Pianura Padana
Emiliana region (northern Italy), causing five deaths and damage to several villages and to …

In the south-eastern corner of the Tyrrhenian basin, in the central Mediterranean Sea, a tight
alignment of earthquakes along a well-defined Benioff zone marks one of the narrowest …

We present the first high-quality catalog of early aftershocks of the three mainshocks of the
2016 central Italy Amatrice-Visso-Norcia normal faulting sequence. We located 10,574 …

Starting from late May 2012, the Emilia region (Northern Italy) was severely shaken by an
intense seismic sequence, originated from a M L 5.9 earthquake on May 20th, at a hypocentral …

In the Ionian Sea (central Mediterranean) the slow convergence between Africa and
Eurasia results in the formation of a narrow subduction zone. The nature of the crust of the …