1-20 OF 256 RESULTS FOR

Amatrice earthquake 2016

Results shown limited to content with bounding coordinates.
Follow your search
Access your saved searches in your account

Would you like to receive an alert when new items match your search?
Close Modal
Sort by
Journal Article
Published: 26 July 2024
Bulletin of the Seismological Society of America (2024) 114 (6): 2823–2845.
...Aybige Akinci; Arben Pitarka; Pietro Artale Harris; Pasquale De Gori; Mauro Buttinelli ABSTRACT The devastating 24 August 2016 M w 6.2 earthquake that struck Amatrice, Italy, marked the beginning of a prolonged seismic sequence dominated by three subsequent M w ≥6.0 events in the central Apennines...
FIGURES
First thumbnail for: Impact of the <span class="search-highlight">Earth...
Second thumbnail for: Impact of the <span class="search-highlight">Earth...
Third thumbnail for: Impact of the <span class="search-highlight">Earth...
Journal Article
Published: 19 July 2024
Seismological Research Letters (2025) 96 (1): 97–110.
...František Čejka; Ľubica Valentová Krišková; Sara Sgobba; Francesca Pacor; František Gallovič Abstract The region of Central Italy is well known for its moderate to large earthquakes. Events such as the 2016 M w 6.2 Amatrice earthquake generated in the shallow extensional tectonic regime motivate...
FIGURES
First thumbnail for: Ground‐Motion Modeling of the <span class="search-...
Second thumbnail for: Ground‐Motion Modeling of the <span class="search-...
Third thumbnail for: Ground‐Motion Modeling of the <span class="search-...
Journal Article
Published: 05 September 2018
Seismological Research Letters (2018) 89 (6): 2227–2236.
...Bruno Hernandez; Alexis Le Pichon; Julien Vergoz; Pascal Herry; Lars Ceranna; Christoph Pilger; Emanuele Marchetti; Maurizio Ripepe; Rémy Bossu ABSTRACT The M w 6.2 Amatrice earthquake that struck central Italy on 24 August 2016 was recorded by seven infrasound arrays in the Euro‐Mediterranean...
FIGURES
First thumbnail for: Estimating the Ground‐Motion Distribution of the <...
Second thumbnail for: Estimating the Ground‐Motion Distribution of the <...
Third thumbnail for: Estimating the Ground‐Motion Distribution of the <...
Journal Article
Published: 13 February 2018
Bulletin of the Seismological Society of America (2018) 108 (2): 553–572.
...Sui Tung; Timothy Masterlark Abstract The source geometry of the 24 August 2016 Amatrice earthquake is studied with Sentinel 1‐A/B and Advanced Land Observation Satellite (ALOS)‐2 Interferometric Synthetic Aperture Radar (InSAR) coseismic observations. Without presetting the fault geometry...
FIGURES
First thumbnail for: Resolving Source Geometry of the 24 August <span c...
Second thumbnail for: Resolving Source Geometry of the 24 August <span c...
Third thumbnail for: Resolving Source Geometry of the 24 August <span c...
Image
RotD50 horizontal SA GOF for simulations of the 2016 Amatrice earthquake using a 3D model with (red lines) and without (black lines) surface topography averaged over recording stations at both groups of distances: (a) stations located within 20 km and (b) stations located beyond 20 km distances. The synthetic seismograms are computed with the preferred rupture model Rup5. The color version of this figure is available only in the electronic edition.
Published: 26 July 2024
Figure 13. RotD50 horizontal SA GOF for simulations of the 2016 Amatrice earthquake using a 3D model with (red lines) and without (black lines) surface topography averaged over recording stations at both groups of distances: (a) stations located within 20 km and (b) stations located beyond 20 km
Image
Slip model of the 2016 Amatrice earthquake and results of the optimization of the broadband model. (a) Slip distribution of the 2016 Mw 6.2 Amatrice earthquake from the dynamic source inversion by Gallovič et al. (2019). The blue star is the nucleation point, gray dots are aftershocks. The red rectangle depicts the area utilized in the Hybrid Integral‐Composite (HIC) modeling. (b) Result of the grid search over parameters a and vr for an optimal model of the 2016 Amatrice earthquake in terms of B2 (top) and σ2 (bottom) values (see equations 2–6). The red square shows the model with minimal B2 with vr=2.45  km/s and a = 1.35. The black line delineates models with the same corner frequency fc as the optimal model (see equation 1). (c) Slip distribution generated for the broadband modeling based on probability density in panel (a). The black triangle is the nucleation point. The color version of this figure is available only in the electronic edition.
Published: 19 July 2024
Figure 2. Slip model of the 2016 Amatrice earthquake and results of the optimization of the broadband model. (a) Slip distribution of the 2016 M w  6.2 Amatrice earthquake from the dynamic source inversion by Gallovič et al. (2019) . The blue star is the nucleation point, gray dots
Journal Article
Published: 25 October 2022
Bulletin of the Seismological Society of America (2022) 112 (6): 3037–3045.
..., namely the Amatrice ( M w 6.0) of 24 August 2016 and the Norcia ( M w 6.5) of 30 October 2016 earthquakes. For this analysis, we used seismograms from the central Italy dense seismic array stations, and earthquakes located at hypocenter distances r < 80 km, having magnitudes M w 3.4–6.5. The dataset...
FIGURES
First thumbnail for: Temporal Variation of the Spectral Decay Parameter...
Second thumbnail for: Temporal Variation of the Spectral Decay Parameter...
Third thumbnail for: Temporal Variation of the Spectral Decay Parameter...
Image
(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 of days elapsed since the Amatrice mainshock of 24 August 2016. The distribution of the seismicity is plotted along two sections, (b) and (c), parallel and perpendicular, respectively, to the average strike of the entire fault system activated during the sequence. The trace of the section parallel to the fault system (b) is indicated in the map (a) by a red line, the trace referred in (c) is just perpendicular to (b) and goes through the epicentral location of the Amatrice earthquake of 24 August 2016 (shown by a yellow star). The color version of this figure is available only in the electronic edition.
Published: 05 June 2025
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 of days
Journal Article
Published: 01 November 2018
Earthquake Spectra (2018) 34 (4): 1671–1691.
... missions: one following the Amatrice Earthquake of 24 August 2016 and one after the end of the earthquake sequence, in May 2017. One objective of the reconnaissance effort was to evaluate existing strengthening methodologies and assess their effectiveness in mitigating the damaging effects of ground...
FIGURES
First thumbnail for: <span class="search-highlight">2016</span>–2017 Ce...
Second thumbnail for: <span class="search-highlight">2016</span>–2017 Ce...
Third thumbnail for: <span class="search-highlight">2016</span>–2017 Ce...
Journal Article
Published: 01 November 2018
Earthquake Spectra (2018) 34 (4): 1721–1737.
... October 2016 event. Recovery strategies related to the bridge collapse near Amatrice, where two temporary bridges were built within 10 days from the first main shock in August, are discussed. An inspected rockfall protection tunnel experienced earthquake pounding effects. In this section, the seismic...
FIGURES
First thumbnail for: Damage to Roadway Infrastructure from <span class=...
Second thumbnail for: Damage to Roadway Infrastructure from <span class=...
Third thumbnail for: Damage to Roadway Infrastructure from <span class=...
Journal Article
Journal: GSA Bulletin
Published: 14 December 2020
GSA Bulletin (2021) 133 (7-8): 1679–1694.
... be carried out considering the seismological data provided, in particular, by the 2009-L′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...
FIGURES
First thumbnail for: The Campotosto linkage fault zone between the 2009...
Second thumbnail for: The Campotosto linkage fault zone between the 2009...
Third thumbnail for: The Campotosto linkage fault zone between the 2009...
Journal Article
Published: 10 July 2025
Bulletin of the Seismological Society of America (2025)
...] and MCMTpy) using real data and by proposing several inversion tests. We selected as test cases two earthquakes belonging to the 2016–2017 central Italy seismic sequence (i.e., the M w 6.0 Amatrice mainshock and an M w 3.2 aftershock) representative of two different magnitude levels. MT solutions obtained...
FIGURES
First thumbnail for: Assessing Double‐Couple Moment Tensor Reliability ...
Second thumbnail for: Assessing Double‐Couple Moment Tensor Reliability ...
Third thumbnail for: Assessing Double‐Couple Moment Tensor Reliability ...
Journal Article
Published: 12 November 2019
Bulletin of the Seismological Society of America (2019) 109 (6): 2738–2740.
...) 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...
Journal Article
Published: 14 March 2024
Bulletin of the Seismological Society of America (2024) 114 (4): 2138–2150.
...František Čejka; Sara Sgobba; Francesca Pacor; Chiara Felicetta; Ľubica Valentová; František Gallovič ABSTRACT The region of central Italy is well known for its moderate‐to‐large earthquakes. Events such as 2016 M w 6.2 Amatrice, generated in the shallow extensional tectonic regime, motivate...
FIGURES
First thumbnail for: Constraining Between‐Event Variability of Kinemati...
Second thumbnail for: Constraining Between‐Event Variability of Kinemati...
Third thumbnail for: Constraining Between‐Event Variability of Kinemati...
Image
Streets in urban nuclei after strong earthquakes: (a) Onna, Italy, 2009, (b) Amatrice, Italy, 2016, and (c) Antakya, Turkey, 2023.
Published: 01 November 2024
Figure 2. Streets in urban nuclei after strong earthquakes: (a) Onna, Italy, 2009, (b) Amatrice, Italy, 2016, and (c) Antakya, Turkey, 2023.
Journal Article
Published: 04 May 2021
The Seismic Record (2021) 1 (1): 11–19.
... Amatrice event on 24 August 2016, followed by the M w 5.9 Visso event on 26 October and the M w 6.5 Norcia event on 30 October. We analyze continuous data from a dense network of 139 seismic stations to build a high‐precision catalog of ∼ 900 , 000 earthquakes spanning a 1 yr period, based on arrival times...
FIGURES
First thumbnail for: Machine‐Learning‐Based High‐Resolution <span class...
Second thumbnail for: Machine‐Learning‐Based High‐Resolution <span class...
Third thumbnail for: Machine‐Learning‐Based High‐Resolution <span class...
Image
Study area and velocity models. (a) Epicentral area of the 2016 Amatrice earthquake with 400 virtual stations (triangles) used for ground‐motion modeling with variable source scenarios. The black curves correspond to the Sibillini thrust separating different crustal regimes of the Norcia and Amatrice area. Colors distinguish velocity models used for stations in the Norcia (blue) and Amatrice areas (red). The black rectangles show the fault planes assumed in the scenario modeling, and focal mechanism plot shows the corresponding mechanism. A map of Italy with the study area depicted by a black rectangle is shown in the inset. (b) Velocity models were used to calculate Green’s functions for stations in the Norcia (blue) and Amatrice (red) area, with inset zooming in the uppermost 1 km. See also Table S1 for the model definitions in numbers. The color version of this figure is available only in the electronic edition.
Published: 14 March 2024
Figure 1. Study area and velocity models. (a) Epicentral area of the 2016 Amatrice earthquake with 400 virtual stations (triangles) used for ground‐motion modeling with variable source scenarios. The black curves correspond to the Sibillini thrust separating different crustal regimes
Journal Article
Journal: GSA Bulletin
Published: 18 July 2024
GSA Bulletin (2025) 137 (1-2): 341–350.
.... Numerical simulations mimic the generation of thermally decomposed fluids and reproduce the 2009 L’Aquila M w 6.3 and the 2016 Amatrice-Visso-Norcia M w 6.5 earthquake sequences. We identify hydraulic barriers and a minimum magnitude (M w > 4) for thermal decomposition, which generate significant...
FIGURES
First thumbnail for: 3-D model reveals thermal decomposition as a poten...
Second thumbnail for: 3-D model reveals thermal decomposition as a poten...
Third thumbnail for: 3-D model reveals thermal decomposition as a poten...
Journal Article
Published: 01 November 2018
Earthquake Spectra (2018) 34 (4): 1547–1555.
... 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...
FIGURES
First thumbnail for: Reconnaissance of <span class="search-highlight">2...
Journal Article
Published: 03 February 2023
Bulletin of the Seismological Society of America (2023) 113 (3): 1208–1229.
...Marta Pischiutta; Rodolfo Puglia; Paola Bordoni; Sara Lovati; Giovanna Cultrera; Alessia Mercuri; Antonio Fodarella; Marco Massa; Ezio D’Alema ABSTRACT Following the M w 6.0 Amatrice earthquake on 24 August 2016 in central Italy, the Emersito task force of the Istituto Nazionale di Geofisica e...
FIGURES
First thumbnail for: Site‐Dependent Amplification on Topography during ...
Second thumbnail for: Site‐Dependent Amplification on Topography during ...
Third thumbnail for: Site‐Dependent Amplification on Topography during ...