Slow slip events (SSEs) represent a slow faulting process leading to aseismic strain release
often accompanied by seismic tremor or earthquake swarms. The larger SSEs last longer …

How, when and where large earthquakes are generated remain fundamental unsolved
scientific questions. Intercepting when a fault system starts deviating from its steady behavior …

The upper part of the Ubaye Valley (French Alps) is characterized by alternating mainshock‐
aftershock sequences and swarms. Particularly, during the 2012–2015 crisis, four …

We performed continuous recordings (May 2015–January 2017) of hydraulic pressure and
electrical conductivity of groundwater in the 190 m-long horizontal S13 borehole drilled next …

How faulting processes lead to a large earthquake is a fundamental question in seismology.
To better constrain this pre‐seismic stage, we create a dense seismic catalog via template …

We use a multidisciplinary approach to gather preliminary evidence for a Quaternary east‐
dip** extensional detachment in Central Italy. This structure crops out in the Sabini …

Tectonic earthquake swarms (TES) often coincide with aseismic slip and sometimes
precede damaging earthquakes. In spite of recent progress in understanding the …

A pilot study employing a template-matching approach on the detection of repeating
earthquakes (or repeaters) in a small volume of the Irpinia fault (Southern Italy) is presented …

We investigate temporal and spatial variations of the spectral decay parameter kappa (κ)
before and after the 6 April 2009, L'Aquila earthquake (M w 6.1), in Central Italy. We …

We investigate the preparatory phase of the 2009, Mw 6.1 L'Aquila earthquake in central
Italy by analyzing the temporal evolution and spatial distribution of the seismic moment, M0 …