Please use this identifier to cite or link to this item:
http://hdl.handle.net/2122/13398
DC Field | Value | Language |
---|---|---|
dc.date.accessioned | 2020-03-06T08:43:08Z | - |
dc.date.available | 2020-03-06T08:43:08Z | - |
dc.date.issued | 2016 | - |
dc.identifier.uri | http://hdl.handle.net/2122/13398 | - |
dc.description.abstract | The thickness of the seismogenic layer is a key parameter for seismic hazard, since it can be used to constrain the maxi- mum depth of faulting and the potential magnitude. In this study, we compute the seismogenic thickness in the Italian region by defining the lower seismicity cut-off, using high- quality hypocentral locations of earthquakes that occurred in the past decade. Along the eastern Alps, the seismogenic thickness is about 12–14 km, laterally homogeneous along the entire south-verging thrust front. In the Apennines exten- sional belt, lateral changes in seismogenic thickness are evi- dent, and correlate with changes in the seismic energy released by past earthquakes. The potential magnitude is lar- ger in the southern Apennines where the seismogenic thick- ness is greater (16–18 km) than in the northern Apennines where it is less (6–10 km) and seismic energy is partially released by the creeping of faults | en_US |
dc.language.iso | English | en_US |
dc.relation.ispartof | Terra Nova | en |
dc.relation.ispartofseries | /28 (2016) | en_US |
dc.title | The seismogenic thickness in Italy: constraints on potential magnitude and seismic hazard | en_US |
dc.type | article | en |
dc.description.status | Published | en_US |
dc.type.QualityControl | Peer-reviewed | en_US |
dc.description.pagenumber | 402-408 | en_US |
dc.identifier.doi | 10.1111/ter.12233 | en_US |
dc.description.obiettivoSpecifico | 4T. Sismicità dell'Italia | en_US |
dc.description.journalType | JCR Journal | en_US |
dc.contributor.author | Chiarabba, Claudio | - |
dc.contributor.author | De Gori, Pasquale | - |
dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia | en_US |
dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia | en_US |
item.openairetype | article | - |
item.cerifentitytype | Publications | - |
item.languageiso639-1 | en | - |
item.grantfulltext | restricted | - |
item.openairecristype | http://purl.org/coar/resource_type/c_18cf | - |
item.fulltext | With Fulltext | - |
crisitem.author.dept | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia | - |
crisitem.author.dept | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia | - |
crisitem.author.orcid | 0000-0002-8111-3466 | - |
crisitem.author.orcid | 0000-0001-8160-0849 | - |
crisitem.author.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
crisitem.author.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
crisitem.department.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
crisitem.department.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
Appears in Collections: | Article published / in press |
Files in This Item:
File | Description | Size | Format | Existing users please Login |
---|---|---|---|---|
seismogenic-crust.pdf | 2.98 MB | Adobe PDF |
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