The 2012 Ferrara seismic sequence: Regional crustal structure, earthquake sources, and seismic hazard
Inadequate seismic design codes can be dangerous, particularly when they underestimate
the true hazard. In this study we use data from a sequence of moderate‐sized earthquakes …
the true hazard. In this study we use data from a sequence of moderate‐sized earthquakes …
The 2012 May 20 and 29, Emilia earthquakes (Northern Italy) and the main aftershocks: S-wave attenuation, acceleration source functions and site effects
We used strong-motion records from the 2012 May 20 and 29 Emilia-Romagna earthquakes
(M w 6.1 and 5.9, respectively) and four aftershocks with magnitudes ranging between 4.9 …
(M w 6.1 and 5.9, respectively) and four aftershocks with magnitudes ranging between 4.9 …
The Ferrara thrust earthquakes of May-June 2012: preliminary site response analysis at the sites of the OGS temporary network
Following the Ml 5.9 earthquake that struck the Emilia area in northern Italy on May 20,
2012, at 02: 03: 53 UTC, and in co-operation with the personnel of the Municipality of …
2012, at 02: 03: 53 UTC, and in co-operation with the personnel of the Municipality of …
The role of aftershocks in the liquefaction phenomena caused by the Emilia 2012 seismic sequence
L Sinatra, S Foti - Soil dynamics and earthquake engineering, 2015 - Elsevier
Extensive and spectacular phenomena of soil liquefaction were observed during the Emilia
seismic sequence that struck northern Italy on May–June 2012. A back-analysis with …
seismic sequence that struck northern Italy on May–June 2012. A back-analysis with …
Integrated dating of the construction and restoration of the Modena cathedral vaults (Northern Italy): preliminary Results
After the last damaging earthquake in 2012, an anti-seismic reinforcement project of the
cathedral of Modena was designed giving us the opportunity to investigate and date the …
cathedral of Modena was designed giving us the opportunity to investigate and date the …
The Earthquake‐Rotated Objects Induced by the 2012 Emilia (Northern Italy) Seismic Sequence: Relation with Seismological and Geomorphological Factors
L Cucci, A Tertulliani - Seismological Research Letters, 2013 - pubs.geoscienceworld.org
In the past few years, the awareness that earthquake-induced rotational effects can be
significant in the near-fault region of an earthquake, and the consequent implications in …
significant in the near-fault region of an earthquake, and the consequent implications in …
[HTML][HTML] Accelerations in the Local Magnetic Field on the Adriatic Tectonic Microplate
R Čop, JL Rasson, A Bilc - Open Journal of Earthquake Research, 2021 - scirp.org
The high level of noise is a special feature of the geomagnetic field on the territory of
Slovenia. The tension of the Adriatic tectonic microplate, on which Slovenia entirely lies, was …
Slovenia. The tension of the Adriatic tectonic microplate, on which Slovenia entirely lies, was …
OGS improvements in 2012 in running the North-eastern Italy Seismic Network: the Ferrara VBB borehole seismic station
D Pesaresi, M Romanelli, C Barnaba… - Advances in …, 2014 - adgeo.copernicus.org
The Centro di Ricerche Sismologiche (CRS, Seismological Research Centre) of the Istituto
Nazionale di Oceanografia e di Geofisica Sperimentale (OGS, Italian National Institute for …
Nazionale di Oceanografia e di Geofisica Sperimentale (OGS, Italian National Institute for …
Installation of a very broad band borehole seismic station in Ferrara (Emilia)
D Pesaresi, L Dall'Olio, A Rovelli… - 31o Convegno …, 2012 - earth-prints.org
The Istituto Nazionale di Geofisica e Vulcanologia (INGV) is the Italian agency devoted to
monitor in real time the seismicity on the Italian territory. The seismicity in Italy is of course …
monitor in real time the seismicity on the Italian territory. The seismicity in Italy is of course …
La sequenza sismica emilian di maggio-giugno 2012–analisi preliminare della risposta di sito nelle stazioni della rete temporanea dell'OGS.
In seguito al terremoto di magnitudo 5.9 che ha colpito la pianura emiliana nord-orientale il
20 maggio 2012 alle 02: 03: 53 UTC, è stata disposta una rete sismica temporanea …
20 maggio 2012 alle 02: 03: 53 UTC, è stata disposta una rete sismica temporanea …