...Arben Pitarka; Aybige Akinci; Pasquale De Gori; Mauro Buttinelli ABSTRACT The M w 6.5 Norcia, Italy, earthquake occurred on 30 October 2016 and caused extensive damage to buildings in the epicentral area. The earthquake was recorded by a network of strong‐motion stations, including 14 stations...

... similar preparatory phases in nature remains difficult because it requires dense monitoring in advance. The 2016 Amatrice-Visso-Norcia (central Italy) earthquake cascade, captured by an unprecedented seismic network, provided a unique testing ground to image the preparatory phase of a large event...

... from near‐source records. The method, based on a piecewise linear detrend of the strong‐motion (SM) recordings, is applied to reconstruct the ground displacement field of the 30 October 2016 M w 6.5 earthquake in central Italy. The robustness of the results is checked against geodetic measurements...

... the application of this scheme to sequences that either conform, or do not, to the MOL behavior, such as the Amatrice–Norcia (Italy 2016–2017), Emilia (Italy 2012), and Tohoku‐Oki (Japan 2011) aftershock sequences. 25 October 2017 © Seismological Society of America Our purpose is to find...

...′Aquila (Mw = 6.3) and the 2016-Amatrice-Visso-Norcia (Mw max = 6.5) earthquakes. Moreover, these high-resolution data, together with the geological surveys carried out immediately after the mainshocks, allowed us to improve our knowledge on the seismotectonic setting of central Italy, and on both...

... to 2016 Central Italy earthquakes of BRB retrofitted school building in Norcia , in Proceedings of the 16th World Conference on Earthquake Engineering, 16WCEE , 9–13 January , Santiago, Chile . Gazzetta Ufficiale , 2003 . Ordinanza del Presidente del Consiglio dei Ministri 20 marzo 2003 n.3274...

...) argue that the negative uplift volume associated with the 2016 Amatrice–Norcia, central Italy, earthquake sequence requires a coseismic volume collapse of the hanging wall. Using results for dip‐slip dislocations in an elastic half‐space we show that V uplift = ( P / 4 ) ( 1 − 2 ν ) sin ( 2 δ...

... earthquakes of L’Aquila (M w 6.1) in 2009 and Norcia (M w 6.5) in 2016 in central Italy. Surprisingly, within this region, fast (≈3 km/s) and destructive seismic ruptures coexist with slow (≤10 m/s) and nondestructive rupture phenomena. Despite its relevance for seismic hazard studies, the transition from...

... Protection). It was followed two months later by an M w  5.9 earthquake near the town of Visso on 26 October, before culminating in an M w  6.5 earthquake near the town of Norcia four days later (Fig.  1 ). The Norcia earthquake is the largest earthquake in Italy since the 1980 M w...

...D. Bindi; D. Spallarossa; M. Picozzi; D. Scafidi; F. Cotton Abstract In this study, we analyzed 10 yrs of seismicity in central Italy from 2008 to 2017, a period witnessing more than 1400 earthquakes in the magnitude range 2.5 ≤ M w ≤ 6.5 . The data set includes the main sequences that have...

...Figure 5. ESM “Event” webpage of the M w  6.5 Norcia (Central Italy) earthquake (see Data and Resources ). The color version of this figure is available only in the electronic edition. ...

... The Central Italy earthquake sequence nominally began on 24 August 2016 with a M 6.1 event on a normal fault that produced devastating effects in the town of Amatrice and several nearby villages and hamlets. A major international response was undertaken to record the effects of this disaster, including...

... that occurred in central Italy from 2008 to 2017 to capture the temporal variability of the ground shaking at high frequency. We first compute between‐event residuals for each earthquake in the Fourier domain with respect to a GMPE developed ad hoc for the analyzed data set. The between‐events show large...