Liquefaction phenomena associated with the Emilia earthquake sequence of May–June 2012 (Northern Italy)

Emergeo Working Group - Natural Hazards and Earth …, 2013 - nhess.copernicus.org
In this paper we present the geological effects induced by the 2012 Emilia seismic sequence
in the Po Plain. Extensive liquefaction phenomena were observed over an area of~ 1200 km …

Blast-induced liquefaction in silty sands for full-scale testing of ground improvement methods: Insights from a multidisciplinary study

S Amoroso, KM Rollins, P Andersen, G Gottardi… - Engineering …, 2020 - Elsevier
In the engineering geology field increased attention has been posed in recent years to
potential liquefaction mitigation interventions in susceptible sand formations. In silty sands …

The first Italian blast-induced liquefaction test 1 (Mirabello, Emilia-Romagna, Italy): Description of the experiment and preliminary results

S Amoroso, G Milana, K Rollins, C Comina… - Annals of …, 2017 - iris.unimore.it
Soil liquefaction can result in significant settlement and reduction of load-bearing capacity.
Moreover, the increase and the accumulation of pore pressure during an earthquake and its …

Liquefaction susceptibility assessment in fluvial plains using airborne lidar: the case of the 2012 Emilia earthquake sequence area (Italy)

R Civico, CA Brunori, PM De Martini… - … Hazards and Earth …, 2015 - nhess.copernicus.org
We report a case study from the Po River plain region (northern Italy), where significant
liquefaction-related land and property damage occurred during the 2012 Emilia seismic …

Palaeoseismological evidence for the 1570 Ferrara earthquake, Italy

R Caputo, ME Poli, L Minarelli, D Rapti, S Sboras… - …, 2016 - Wiley Online Library
Abstract In May 2012, two earthquakes (Mw 6.1 and 5.9) affected the Po Plain, Italy. The
strongest shock produced extensive secondary effects associated with liquefaction …

The influence of alluvial stratigraphic architecture on liquefaction phenomena: a case study from the Terre del Reno subsoil (southern Po plain, Italy)

D Tentori, M Mancini, C Varone, R Spacagna… - Sedimentary …, 2022 - Elsevier
Earthquake-induced liquefaction phenomena are commonly observed at shallow depths or
at the ground surface above Holocene alluvial deposits. Nonetheless, a high-resolution …

The LVD signals during the early-mid stages of the L'Aquila seismic sequence and the radon signature of some aftershocks of moderate magnitude

C Cigolini, M Laiolo, D Coppola - Journal of Environmental Radioactivity, 2015 - Elsevier
The L'Aquila seismic swarm culminated with the mainshock of April 6, 2009 (ML= 5.9). Here,
we report and analyze the Large Volume Detector (LVD, used in neutrinos research) low …

Geological reconstruction in the area of maximum co-seismic subsidence during the 2009 Mw= 6.1 L'Aquila earthquake using geophysical and borehole data

M Porreca, A Smedile, F Speranza… - Italian Journal of …, 2016 - pubs.geoscienceworld.org
InSAR images showed that the 2009 Mw= 6.1 normal faulting L'Aquila earthquake (Abruzzi
region, central Italy) produced a maximum co-seismic subsidence of ca. 24 cm in the …

A detailed liquefaction susceptibility map of nestos river delta, thrace, Greece based on surficial geology and geomorphology

M Taftsoglou, S Valkaniotis, G Papathanassiou… - Geosciences, 2022 - mdpi.com
The existence of high potential onshore and offshore active faults capable to trigger large
earthquakes in the broader area of Thrace, Greece in correlation with the critical …

Main geologic factors controlling site response during the 2009 L'Aquila earthquake

L Martelli, P Boncio, M Baglione… - Italian Journal of …, 2012 - pubs.geoscienceworld.org
Main geologic factors controlling site response during the 2009 L’Aquila earthquake | Italian
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