Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/9240
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dc.contributor.authorallSciarra, A.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.authorallCantucci, B.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.authorallAbu Zeid, N.; Dipartimento di Fisica e Scienze della Terra, Università di Ferrara,en
dc.contributor.authorallVaccaro, C.; Dipartimento di Fisica e Scienze della Terra, Università di Ferrara,en
dc.contributor.authorallQuattrocchi, F.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.editorallLollino, G:en
dc.date.accessioned2015-01-12T10:51:23Zen
dc.date.available2015-01-12T10:51:23Zen
dc.date.issued2014en
dc.identifier.urihttp://hdl.handle.net/2122/9240en
dc.description.abstractOn May 20th and 29th, 2012 two earthquakes (ML 5.9 with hypocenter depth at 6.3 km and ML 5.8 with hypocenter depth at 10.2 km, respectively; ISIDe Database) struck the Emilia area. The epicentre was located in the vicinity of Finale Emilia and Medolla (Modena). Co-seismic effects exemplified by liquefactions and surface ruptures occurred in the surrounding area (Provinces of Bologna, Ferrara, Modena, Reggio Emilia, Mantova and Rovigo). The maximum effects where concentrated along the towns located 15–25 km from the epicentre (SW portion of Ferrara Province). Soon after the main events, several geochemical and geophysical surveys were carried out in different sites at Modena and Ferrara Provinces, where surface rupture and liquefaction effects were most evident. Results gained from soil and dissolved gases and geoelectrical-geophysical surveys evidenced that the main liquefied layer is related to a medium coarse-grained sand saturated aquifer located at 8–12 m b.g.l. On the other hand, superficial unsaturated sediments underwent liquefaction represented by densification and lateral spreading. As a consequence, liquefied soil caused ground failures and damages to the built environment. The extent of the liquefaction phenomena, its concentration along the Reno paleo-river ridge and the building damage, has highlighted the need to further characterized the possible rule of lithology and natural gas content on the outset of liquefaction.en
dc.language.isoEnglishen
dc.relation.ispartofEngineering Geology for Society and Territoryen
dc.relation.ispartofseries5en
dc.subjectLiquefactionen
dc.subjectsurface ruptureen
dc.subjectsoil gasen
dc.subjectelectrical resistivity tomographyen
dc.subjectinduced polarizationen
dc.titleGeochemical and Geomorphological Analyses on Liquefaction Occurred During the 2012 Emilia Seismic Sequenceen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.subject.INGV05. General::05.02. Data dissemination::05.02.01. Geochemical dataen
dc.identifier.doi10.1007/978-3-319-09048-1_183en
dc.description.obiettivoSpecifico2T. Tettonica attivaen
dc.description.journalTypeN/A or not JCRen
dc.publisherSPRINGERen
dc.description.fulltextrestricteden
dc.contributor.authorSciarra, A.en
dc.contributor.authorCantucci, B.en
dc.contributor.authorAbu Zeid, N.en
dc.contributor.authorVaccaro, C.en
dc.contributor.authorQuattrocchi, F.en
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.departmentDipartimento di Fisica e Scienze della Terra, Università di Ferrara,en
dc.contributor.departmentDipartimento di Fisica e Scienze della Terra, Università di Ferrara,en
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.editorLollino, G:en
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextrestricted-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia-
crisitem.author.deptUniversità di Ferrara, Dipartimento di Scienze della Terra-
crisitem.author.deptDipartimento di Fisica e Scienze della Terra, Università di Ferrara,-
crisitem.author.orcid0000-0003-3767-3105-
crisitem.author.orcid0000-0001-7266-5106-
crisitem.author.orcid0000-0002-7822-1394-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent05. General-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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