The 2016 central Italy seismic sequence: A first look at the mainshocks, aftershocks, and source models
The 2016 central Italy seismic sequence consists so far of a series of moderate‐to‐large
earthquakes activating within a few months along a 60‐km‐long and Apenninic‐trending …
earthquakes activating within a few months along a 60‐km‐long and Apenninic‐trending …
Machine‐learning‐based high‐resolution earthquake catalog reveals how complex fault structures were activated during the 2016–2017 central Italy sequence
The 2016–2017 central Italy seismic sequence occurred on an 80 km long normal‐fault
system. The sequence initiated with the M w 6.0 Amatrice event on 24 August 2016, followed …
system. The sequence initiated with the M w 6.0 Amatrice event on 24 August 2016, followed …
[HTML][HTML] The influence of subsurface geology on the distribution of earthquakes during the 2016‐–2017 Central Italy seismic sequence
Abstract In 2016–2017, a destructive sequence of earthquakes affected a wide portion of
Central Italy, activating a complex, 80-km long system of SW-dipping normal faults and …
Central Italy, activating a complex, 80-km long system of SW-dipping normal faults and …
Multi-segment rupture of the 2016 Amatrice-Visso-Norcia seismic sequence (central Italy) constrained by the first high-quality catalog of Early Aftershocks
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 …
2016 central Italy Amatrice-Visso-Norcia normal faulting sequence. We located 10,574 …
Lithospheric double shear zone unveiled by microseismicity in a region of slow deformation
R de Nardis, C Pandolfi, M Cattaneo, G Monachesi… - Scientific Reports, 2022 - nature.com
The deformation style of the continental lithosphere is a relevant issue for geodynamics and
seismic hazard perspectives. Here we show the first evidence of two well-distinct low-angle …
seismic hazard perspectives. Here we show the first evidence of two well-distinct low-angle …
Fine‐scale structure of the 2016–2017 Central Italy seismic sequence from data recorded at the Italian National Network
We explore the three‐dimensional structure of the 2016–2017 Central Italy sequence using~
34,000 ML≥ 1.5 earthquakes that occurred between August 2016 and January 2018. We …
34,000 ML≥ 1.5 earthquakes that occurred between August 2016 and January 2018. We …
Surface and crustal response to deep subduction dynamics: Insights from the Apennines, Italy
The topography of orogenic belts responds to several contributions operating at short and
long temporal and spatial (ie, wavelengths) scales, from the surface to the deep mantle …
long temporal and spatial (ie, wavelengths) scales, from the surface to the deep mantle …
Lakes as paleoseismic records in a seismically-active, low-relief area (Rieti Basin, central Italy)
Small lakes in low relief areas are atypical candidates for studies on paleoseismicity, but
their sediments can contain seismically induced event layers (seismites) generated through …
their sediments can contain seismically induced event layers (seismites) generated through …
Fault planes, fault zone structure and detachment fragmentation resolved with high‐precision aftershock locations of the 2016–2017 central Italy sequence
Three devastating earthquakes of MW≥ 5.9 activated a complex system of high‐angle
normal, antithetic, and sub‐horizontal detachment faults during the 2016–2017 central Italy …
normal, antithetic, and sub‐horizontal detachment faults during the 2016–2017 central Italy …
Large earthquakes driven by fluid overpressure: The Apennines normal faulting system case
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 …
triggering. The Apennines section within the young Alpine mobile belt is a key locus to …