Quantitative Estimate of the Long-Term Slip Rate of the Normal Fault Responsible for the 2009 L’Aquila Earthquake (Mw 6.1) (Central Italy) Through Tectonic Geomorphology Approaches

2021 ◽  
Author(s):  
Irene Puliti ◽  
Stefano Pucci ◽  
Fabio Villani ◽  
Massimiliano Porreca ◽  
Lucilla Benedetti ◽  
...  
Keyword(s):  
Quantitative Estimate ◽  
Central Italy ◽  
Slip Rate ◽  
Normal Fault ◽  
Tectonic Geomorphology ◽  
L’Aquila Earthquake ◽  
2009 L’Aquila Earthquake

scholarly journals Long-term blood pressure changes induced by the 2009 L’Aquila earthquake: assessment by 24h ambulatory monitoring

2013 ◽  
Vol 36 (9) ◽  
pp. 795-798 ◽  
Author(s):  
Paolo Giorgini ◽  
Rinaldo Striuli ◽  
Marco Petrarca ◽  
Luisa Petrazzi ◽  
Paolo Pasqualetti ◽  
...  
Keyword(s):  
Blood Pressure ◽  
Ambulatory Monitoring ◽  
L’Aquila Earthquake ◽  
2009 L’Aquila Earthquake ◽  
Pressure Changes ◽  
Earthquake Assessment

Impact of the 6 April 2009 L'Aquila earthquake on groundwater flow in the Gran Sasso carbonate aquifer, Central Italy

2010 ◽  
Vol 25 (11) ◽  
pp. 1754-1764 ◽  
Author(s):  
Antonella Amoruso ◽  
Luca Crescentini ◽  
Marco Petitta ◽  
Sergio Rusi ◽  
Marco Tallini
Keyword(s):  
Groundwater Flow ◽  
Central Italy ◽  
L’Aquila Earthquake ◽  
Carbonate Aquifer ◽  
2009 L’Aquila Earthquake

scholarly journals Coseismic ground deformation of the 6 April 2009 L'Aquila earthquake (central Italy, Mw6.3)

2010 ◽  
Vol 37 (6) ◽  
pp. n/a-n/a ◽  
Author(s):  
P. Boncio ◽  
A. Pizzi ◽  
F. Brozzetti ◽  
G. Pomposo ◽  
G. Lavecchia ◽  
...  
Keyword(s):  
Ground Deformation ◽  
Central Italy ◽  
L’Aquila Earthquake ◽  
2009 L’Aquila Earthquake

scholarly journals The 2009 L'Aquila earthquake (central Italy): A source mechanism and implications for seismic hazard

2009 ◽  
Vol 36 (17) ◽  
Author(s):  
R. J. Walters ◽  
J. R. Elliott ◽  
N. D'Agostino ◽  
P. C. England ◽  
I. Hunstad ◽  
...  
Keyword(s):  
Seismic Hazard ◽  
Central Italy ◽  
Source Mechanism ◽  
L’Aquila Earthquake ◽  
2009 L’Aquila Earthquake

scholarly journals Recent seismicity before the 24 August 2016 Mw 6.0 Central Italy Earthquake as recorded by the ReSIICO seismic network

2016 ◽  
Vol 59 ◽  
Author(s):  
Simone Marzorati ◽  
Marco Cattaneo ◽  
Massimo Frapiccini ◽  
Giancarlo Monachesi ◽  
Chiara Ladina
Keyword(s):  
Central Italy ◽  
Seismic Network ◽  
Seismic Sequence ◽  
L’Aquila Earthquake ◽  
Preliminary Results ◽  
Seismic Sequences ◽  
Seismic Swarm ◽  
Central Italy Earthquake ◽  
2009 L’Aquila Earthquake ◽  
Preparatory Phase

The seismicity of the last four years before the August 24 2016 01:36 UTC M<sub>W</sub> 6.0 earthquake that struck central Italy is presented with the aim to understand the preparatory phase of the event. In contrast with the 2009 L’Aquila earthquake that was preceded by a seismic sequence and the 2013-2015 Gubbio seismic swarm that, to date, is ended without any strong event, our preliminary results don’t show seismic sequences in the last months previous the mainshock of the August 24 2016 and a low similarity between seismicity clusters in the last four years and the foreshocks.

scholarly journals Late Quaternary faulting in southern Matese (central Italy): implications for earthquake potential in the southern Apennines

2021 ◽  
Author(s):  
Paolo Boncio ◽  
Eugenio Auciello ◽  
Vincenzo Amato ◽  
Pietro Aucelli ◽  
Paola Petrosino ◽  
...  
Keyword(s):  
Late Quaternary ◽  
Central Italy ◽  
Slip Rate ◽  
Normal Fault ◽  
Historical Earthquakes ◽  
Fault System ◽  
Southern Apennines ◽  
Mountain Front ◽  
Point Data ◽  
Earthquake Potential

Abstract. We studied in detail the Gioia Sannitica active normal fault (GF) along the Southern Matese Fault system in the southern Apennines of Italy. The current activity of the fault system and its potential to produce strong earthquakes have been underestimated so far, and are now defined. Precise mapping of the GF fault trace on a 1 : 20,000 geological map and several point data on geometry, kinematics and throw rate are made available in electronic format. The GF, and in general the entire fault system along the southern Matese mountain front, is made of slowly-slipping faults, with a long active history revealed by the large geologic offsets, mature geomorphology, and complex fault pattern and kinematics. Present activity has resulted in Late Quaternary fault scarps resurrecting the foot of the mountain front, and Holocene surface faulting. The slip rate varies along-strike, with maximum Late Pleistocene – Holocene throw rate of ~0.5 mm/yr. Activation of the 11.5 km-long GF can produce up to M 6.1 earthquakes. If activated together with the 18 km-long Ailano-Piedimonte Matese fault (APMF), the seismogenic potential would be M 6.8. The slip history of the two faults is compatible with a contemporaneous rupture. The observed Holocene displacements on the GF and APMF are compatible with activations during some poorly known historical earthquakes, such as the 1293 (M 5.8), 1349 (M 6.8; southern prolongation of the rupture on the Aquae Iuliae fault?) and CE 346 earthquakes. A fault rupture during the 847 poorly-constrained historical earthquake is also compatible with the dated displacements.

scholarly journals Coseismic deformation of the destructive April 6, 2009 L'Aquila earthquake (central Italy) from GPS data

2009 ◽  
Vol 36 (17) ◽  
Author(s):  
M. Anzidei ◽  
E. Boschi ◽  
V. Cannelli ◽  
R. Devoti ◽  
A. Esposito ◽  
...  
Keyword(s):  
Central Italy ◽  
Coseismic Deformation ◽  
Gps Data ◽  
L’Aquila Earthquake ◽  
2009 L’Aquila Earthquake
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