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Visso Italy

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Journal Article
Journal: GSA Bulletin
Published: 14 December 2020
GSA Bulletin (2021) 133 (7-8): 1679–1694.
... may be better understood considering the recent results on rupture directivity provided by Calderoni et al. (2017) for sixteen earthquakes of Mw > 4.4 belonging to the 2016 Amatrice-Norcia-Visso seismic sequences. The seismic sequences that occurred in the last decades in central Italy...
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Journal Article
Published: 01 May 2018
Bulletin of the Seismological Society of America (2018) 108 (3A): 1427–1442.
...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...
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Journal Article
Journal: GSA Bulletin
Published: 18 July 2024
GSA Bulletin (2025) 137 (1-2): 341–350.
... in these overlapping sequences (yellow box) and is shown in Figure S2. Figure 1. Epicenters of 55,000 events from the 2009 L’Aquila sequence (coded by depth in gray) and the 2016 AVN sequence (coded by depth in green) in the Apennines of Italy. The two earthquake sequences that span the area between Visso...
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Image
Photos of the buildings considered in this study: (a) Aviano, (b) Cividale, (c) Fogliano, (d) Gemona, (e) Gorizia, (f) Ronchi dei Legionari, (g) Tarvisio, (h) Tolmezzo and Visso (central Italy, panels i and j, respectively, for front and back view), and examples of installations at the bottom and top of the Aviano building (panels k and l, respectively). All photos with the exception of (i) and (j) are extracted from the Armonia project internal documentation. (i,j) The images of Visso school are extracted from the Osservatorio Sismico delle Strutture (OSS) documentation. The color version of this figure is available only in the electronic edition.
Published: 27 February 2023
Figure 1. Photos of the buildings considered in this study: (a) Aviano, (b) Cividale, (c) Fogliano, (d) Gemona, (e) Gorizia, (f) Ronchi dei Legionari, (g) Tarvisio, (h) Tolmezzo and Visso (central Italy, panels i and j, respectively, for front and back view), and examples of installations
Journal Article
Published: 10 April 2023
Seismological Research Letters (2023) 94 (4): 1912–1924.
... without requiring the deconvolution of the instrumental response and without knowing a priori the attenuation model and the orientation of the activated fault system. We apply the method to the 2016–2017 Amatrice‐Visso‐Norcia high‐energy and long‐lasting earthquake series in central Italy, which affected...
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Journal Article
Published: 04 May 2021
The Seismic Record (2021) 1 (1): 11–19.
... 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...
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Image
- Geological sketch map of the Umbria-Marche Apennines (modified after Pierantoni et al., 2013). Black and red boxes show location of Sheet 325-Visso of the geological map of Italy and the study area, respectively.
Published: 01 October 2023
Fig. 1 - Geological sketch map of the Umbria-Marche Apennines (modified after Pierantoni et al., 2013 ). Black and red boxes show location of Sheet 325-Visso of the geological map of Italy and the study area, respectively.
Journal Article
Journal: Geology
Published: 01 June 2020
Geology (2020) 48 (9): 924–928.
... 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...
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Journal Article
Published: 29 March 2017
Seismological Research Letters (2017) 88 (3): 757–771.
...L. Chiaraluce; R. Di Stefano; E. Tinti; L. Scognamiglio; M. Michele; E. Casarotti; M. Cattaneo; P. De Gori; C. Chiarabba; G. Monachesi; A. Lombardi; L. Valoroso; D. Latorre; S. Marzorati ABSTRACT The 2016 central Italy seismic sequence consists so far of a series of moderate‐to‐large earthquakes...
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Image
Spatial distribution of hypocenters in the Apennines of Italy superposed on the calculated fluid pressure field. (A) The top view shows a strong correlation between regions of calculated high-pressure fluids and the hypocentral distribution for all sections. (B) Same data and model results shown in 3-D perspective also showing a clear correlation with calculated fluid overpressures. AVN—Amatrice-Visso-Norcia.
Published: 18 July 2024
Figure 4. Spatial distribution of hypocenters in the Apennines of Italy superposed on the calculated fluid pressure field. (A) The top view shows a strong correlation between regions of calculated high-pressure fluids and the hypocentral distribution for all sections. (B) Same data and model
Journal Article
Published: 27 February 2023
Seismological Research Letters (2023) 94 (3): 1536–1555.
...Figure 1. Photos of the buildings considered in this study: (a) Aviano, (b) Cividale, (c) Fogliano, (d) Gemona, (e) Gorizia, (f) Ronchi dei Legionari, (g) Tarvisio, (h) Tolmezzo and Visso (central Italy, panels i and j, respectively, for front and back view), and examples of installations...
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Journal Article
Published: 25 October 2022
Bulletin of the Seismological Society of America (2022) 112 (6): 3037–3045.
... correspond to the epicenters of the M w  6.0 Amatrice (42°42′ N, 13°13.8′ E), the M w  5.9 Visso (42°54.6′ N, 13°7.8′ E), and the M w  6.5 Norcia (42°49.8′ N, 13°6.6′ E) earthquakes. The top right inset shows a regional map of the location in central Italy (shown with the red...
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Image
Epicenters of 55,000 events from the 2009 L’Aquila sequence (coded by depth in gray) and the 2016 AVN sequence (coded by depth in green) in the Apennines of Italy. The two earthquake sequences that span the area between Visso and L’Aquila are associated with three dominant geological domains. These include Lazio-Abruzzo, Umbria-Marche, and the Laga Formation (see legend). The yellow box indicates the overlap between the 2009 L’Aquila and 2016 AVN sequences and expanded in Figure S2 (see text footnote 1).
Published: 18 July 2024
Figure 1. Epicenters of 55,000 events from the 2009 L’Aquila sequence (coded by depth in gray) and the 2016 AVN sequence (coded by depth in green) in the Apennines of Italy. The two earthquake sequences that span the area between Visso and L’Aquila are associated with three dominant geological
Journal Article
Published: 05 June 2025
Bulletin of the Seismological Society of America (2025)
.... , 2006). Figure 2. (a) Map of the area affected by the 2016–2017 Amatrice–Visso–Norcia–Capitignano earthquake sequence, showing the distribution of all events with magnitude M  2.5+. The inset indicates the exact location of the study area (the white rectangle). The coloring indicates the number...
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Journal Article
Published: 29 October 2024
Bulletin of the Seismological Society of America (2025) 115 (3): 983–999.
...Dino Bindi; Daniele Spallarossa; Matteo Picozzi; Gabriele Tarchini ABSTRACT We study the scaling between seismic moment and corner frequency, and the spatial variability of the stress drop, in central and southern Italy. We analyze a data set generated by 28,943 earthquakes that occurred between...
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Journal Article
Published: 01 February 2022
Earthquake Spectra (2022) 38 (1): 702–724.
... before the M w 5.9, and availability of temporary accommodation, the populations suffered no additional casualties during these events. The Norcia event was located between the Amatrice and Visso earthquakes, causing some of the most impressive surface faulting ever seen in Italy. In January 2017...
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Image
Graphical representation of the equivalent magnitude of the central Apennines fault system-related historical earthquakes of central Italy versus time and seismic cycle (modified after Tondi and Cello, 2003). The cumulative displacements for the 2009 L′Aquila and 2016 Amatrice-Visso-Norcia earthquakes are from Cheloni et al. (2014) and Walters et al. (2018). The historical earthquakes reported in the table are those originally included in Tondi and Cello (2003) based on seismic catalogues cited therein. Imax—maximum intensity; Me—equivalent magnitude; Mw—moment magnitude.
Published: 14 December 2020
Figure 7. Graphical representation of the equivalent magnitude of the central Apennines fault system-related historical earthquakes of central Italy versus time and seismic cycle (modified after Tondi and Cello, 2003 ). The cumulative displacements for the 2009 L′Aquila and 2016 Amatrice-Visso
Image
(a) Maps of the distribution of earthquakes analyzed with magnitudes ranging between 3.4 and 6.5. The red stars correspond to the epicenters of the Mw 6.0 Amatrice (42°42′ N, 13°13.8′ E), the Mw 5.9 Visso (42°54.6′ N, 13°7.8′ E), and the Mw 6.5 Norcia (42°49.8′ N, 13°6.6′ E) earthquakes. The top right inset shows a regional map of the location in central Italy (shown with the red rectangle). (b) Map with recording stations. The color version of this figure is available only in the electronic edition.
Published: 25 October 2022
Figure 1. (a) Maps of the distribution of earthquakes analyzed with magnitudes ranging between 3.4 and 6.5. The red stars correspond to the epicenters of the M w  6.0 Amatrice (42°42′ N, 13°13.8′ E), the M w  5.9 Visso (42°54.6′ N, 13°7.8′ E), and the M w  6.5 Norcia (42
Image
3-D model of the seismogenic structures related to the 2009 L′Aquila seismic sequence (purple) and the 2016–2017 Amatrice-Visso-Norcia seismic sequence (red/brown) of central Italy. The model shows the difference in length between the capable faults at the surface and the related seismogenic sources at depth. This difference is consistent with the pronounced elliptical shape typical of normal faults (Torabi et al., 2019). The seismogenic sources of the main events (moment magnitude ≥ 5.0) that occurred in the underlap region between the two main faults outline a linkage zone beneath the Campotosto area.
Published: 14 December 2020
Figure 8. 3-D model of the seismogenic structures related to the 2009 L′Aquila seismic sequence (purple) and the 2016–2017 Amatrice-Visso-Norcia seismic sequence (red/brown) of central Italy. The model shows the difference in length between the capable faults at the surface and the related
Journal Article
Journal: Geology
Published: 14 August 2023
Geology (2023) 51 (10): 988–992.
.... The 2016–2017 Central Italy seismic sequence started on 24 August 2016 with the Amatrice M w = 6.0 earthquake ( Fig. 1A ). This first main shock was followed by two other large earthquakes: the M w = 5.9 Visso and M w = 6.5 Norcia earthquakes on 26 and 30 October, respectively. On 18 January 2017, the M...
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