Repeating earthquakes, or repeaters, are identical in location and geometry but occur at
different times. They appear to represent recurring seismic energy release from distinct …

Modern geodetic and seismologic observations describe the behavior of fault slip over a
vast range of spatial and temporal scales. Slip at sub-seismogenic speeds is evident from …

Abstract Analysis of seismicity can illuminate active fault zone structures but also
deformation within large volumes of the seismogenic zone. For the Mw 6.5 2016–2017 …

Despite a lack of modern large earthquakes on shallowly dip** normal faults, Holocene
Mw> 7 low-angle normal fault (LANF; dip< 30°) ruptures are preserved paleoseismically and …

Fluid overpressure is a primary mechanism behind fault interaction and earthquakes
triggering. The Apennines section within the young Alpine mobile belt is a key locus to …

The integration of field geology and high-resolution seismological data allowed us to
reconstruct the 3D Fault Model of the sources which gave rise to the 2010–2014 Pollino …

Abstract The Alto Tiberina Fault system, located in the Northern Apennines (Italy), consists of
a low angle normal fault (LANF) which radiates micro‐seismicity that can be explained by …

The Near Fault Observatories (NFOs) community is one of the European Plate Observing
System (EPOS, http://www. epos-eu. org) Thematic Communities, today consisting of six …

The evolution and state of geological structure at Earth's surface is best understood with an
accurate characterization of the subsurface. Here we present seismic tomographic images of …

This paper presents a novel methodology for earthquake-induced damage identification of
historical constructions through sparse multivariate regression. The proposed methodology …