Search engine for discovering works of Art, research articles, and books related to Art and Culture
ShareThis
Javascript must be enabled to continue!

What is the impact of the August 24, 2016 Amatrice earthquake on the seismic hazard assessment in central Italy?

View through CrossRef
<p>The recent Amatrice strong event (M<sub>w</sub>6.0) occurred on August 24, 2016 in Central Apennines (Italy) in a seismic gap zone, motivated us to study and provide better understanding of the seismic hazard assessment in the macro area defined as “Central Italy”. The area affected by the sequence is placed between the M<sub>w</sub>6.0 1997 Colfiorito sequence to the north (Umbria-Marche region) the Campotosto area hit by the 2009 L’Aquila sequence M<sub>w</sub>6.3 (Abruzzo region) to the south. The Amatrice earthquake occurred while there was an ongoing effort to update the 2004 seismic hazard map (MPS04) for the Italian territory, requested in 2015 by the Italian Civil Protection Agency to the Center for Seismic Hazard (CPS) of the Istituto Nazionale di Geofisica e Vulcanologia INGV. Therefore, in this study we brought to our attention new earthquake source data and recently developed ground-motion prediction equations (GMPEs). Our aim was to validate whether the seismic hazard assessment in this area has changed with respect to 2004, year in which the MPS04 map was released. In order to understand the impact of the recent earthquakes on the seismic hazard assessment in central Italy we compared the annual seismic rates calculated using a smoothed seismicity approach over two different periods; the Parametric Catalog of the Historical Italian earthquakes (CPTI15) from 1871 to 2003 and the historical and instrumental catalogs from 1871 up to 31 August 2016. Results are presented also in terms of peak ground acceleration (PGA), using the recent ground-motion prediction equations (GMPEs) at Amatrice, interested by the 2016 sequence.</p>
Title: What is the impact of the August 24, 2016 Amatrice earthquake on the seismic hazard assessment in central Italy?
Description:
<p>The recent Amatrice strong event (M<sub>w</sub>6.
0) occurred on August 24, 2016 in Central Apennines (Italy) in a seismic gap zone, motivated us to study and provide better understanding of the seismic hazard assessment in the macro area defined as “Central Italy”.
The area affected by the sequence is placed between the M<sub>w</sub>6.
0 1997 Colfiorito sequence to the north (Umbria-Marche region) the Campotosto area hit by the 2009 L’Aquila sequence M<sub>w</sub>6.
3 (Abruzzo region) to the south.
The Amatrice earthquake occurred while there was an ongoing effort to update the 2004 seismic hazard map (MPS04) for the Italian territory, requested in 2015 by the Italian Civil Protection Agency to the Center for Seismic Hazard (CPS) of the Istituto Nazionale di Geofisica e Vulcanologia INGV.
Therefore, in this study we brought to our attention new earthquake source data and recently developed ground-motion prediction equations (GMPEs).
Our aim was to validate whether the seismic hazard assessment in this area has changed with respect to 2004, year in which the MPS04 map was released.
In order to understand the impact of the recent earthquakes on the seismic hazard assessment in central Italy we compared the annual seismic rates calculated using a smoothed seismicity approach over two different periods; the Parametric Catalog of the Historical Italian earthquakes (CPTI15) from 1871 to 2003 and the historical and instrumental catalogs from 1871 up to 31 August 2016.
Results are presented also in terms of peak ground acceleration (PGA), using the recent ground-motion prediction equations (GMPEs) at Amatrice, interested by the 2016 sequence.
</p>.

Related Results

Analysis of Seismic Cycle Deformation for the Ms7.1 Wushi Earthquake in Xinjiang Based on Geodetic Data
Analysis of Seismic Cycle Deformation for the Ms7.1 Wushi Earthquake in Xinjiang Based on Geodetic Data
On January 23, 2024, an Ms7.1 earthquake struck Wushi County, Aksu Prefecture, Xinjiang. While resulting in relatively limited casualties and economic losses, the event posed a cer...
Instrumental seismicity of the Amatrice earthquake epicentral area: a review 
Instrumental seismicity of the Amatrice earthquake epicentral area: a review 
<p><em>This study presents a review of the instrumental seismicity of the Norcia-Amatrice area (central Italy) where a still on-going seismic sequence started on August...
Penerapan Sequence Probabilistic Seismic Hazard Analysis dalam Pemodelan Seismogenic Hazard
Penerapan Sequence Probabilistic Seismic Hazard Analysis dalam Pemodelan Seismogenic Hazard
Abstract. Seismogenic areas are areas in the earth's crust that have the potential to produce seismic waves due to tectonic activity. Identification of a seismogenic area measuring...
Microseismic characterization of Fribourg area (Switzerland) by nanoseismic monitoring
Microseismic characterization of Fribourg area (Switzerland) by nanoseismic monitoring
This thesis aims to investigate the present level of microseismicity generated within the Fribourg area (Switzerland). In particular, it focuses on a 20- 30 km N-S trending seismic...
4D Seismic on Gullfaks
4D Seismic on Gullfaks
SUMMARY New technologies are rapidly emerging helping to obtain optimal drainage of large reservoirs. 4D seismic is such a reservoir monitoring technique. The phy...
Seismic Frequency Enhancement for Mapping and Reservoir Characterization of Arab Formation: Case Study Onshore UAE
Seismic Frequency Enhancement for Mapping and Reservoir Characterization of Arab Formation: Case Study Onshore UAE
Abstract Mapping and discrimination of Upper Jurassic Arab reservoirs (Arab A/B/C and D) in this 3D seismic onshore field of Abu Dhabi, is very sensitive to the seis...
Development of the new seismic network of the IGS, Armenia
Development of the new seismic network of the IGS, Armenia
The Republic of Armenia and the neighboring areas are located in the central part of theArabia-Eurasia collision zone, which is characterized by active seismicity.Over the past dec...
Estimation of earthquake size for seismic hazards
Estimation of earthquake size for seismic hazards
Abstract This chapter presents a structured organization of the various types of seismic-hazard estimates, approaches, scaling parameters, techniques, and data used ...

Back to Top