Please use this identifier to cite or link to this item:
http://hdl.handle.net/2122/5131
DC Field | Value | Language |
---|---|---|
dc.contributor.authorall | Di Bucci, D.; P.C.M. - Dipartimento della Protezione Civile, 00189 Roma | en |
dc.contributor.authorall | Ridente, D.; Istituto di Geologia Ambientale e Geoingegneria, CNR, 00185 Roma | en |
dc.contributor.authorall | Fracassi, U.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italia | en |
dc.contributor.authorall | Trincardi, F.; Istituto di Scienze Marine, CNR, 40129 Bologna | en |
dc.contributor.authorall | Valensise, G.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italia | en |
dc.date.accessioned | 2009-07-23T06:41:42Z | en |
dc.date.available | 2009-07-23T06:41:42Z | en |
dc.date.issued | 2009 | - |
dc.identifier.uri | http://hdl.handle.net/2122/5131 | en |
dc.description.abstract | We present a marine paleoseismology analysis of a dense network of very high resolution seismic profiles along the Gondola Fault Zone (GFZ), a right-lateral, E-W–striking, active fault system in the Adriatic foreland. This case-study aims to show how time and space variations in the activity of a dominantly right-lateral fault system can be assessed based on the vertical component of slip alone. The GFZ has been investigated for a length of 50 km. It includes two parallel subvertical fault sets and two main anticlines. The distribution of the late Middle Pleistocene to Holocene vertical component of displacement along-fault is bell-shaped, suggesting that in the long-term the fault zone acts as a single, kinematically coherent structure. Slip rates on individual fault segments, however, suggest that they may rupture independently. Vertical slip rates calculated for late Middle Pleistocene-Holocene intervals fall in a narrow range and are consistently small (0-0.18 mm/a). | en_US |
dc.language.iso | English | en_US |
dc.publisher.name | Wiley - Blackwell | en_US |
dc.relation.ispartof | Terra Nova | en |
dc.relation.ispartofseries | 5/ 21 (2009) | en_US |
dc.subject | Chirp-Sonar profiles | en_US |
dc.subject | fault reactivation | en_US |
dc.subject | right-lateral shear | en_US |
dc.subject | Adriatic Sea | en_US |
dc.subject | Italy | en_US |
dc.title | Marine paleoseismology from Very High Resolution seismic imaging: the Gondola Fault Zone (Adriatic foreland) | en_US |
dc.type | article | en_US |
dc.description.status | Published | en_US |
dc.type.QualityControl | Peer-reviewed | en_US |
dc.description.pagenumber | 393-400 | en_US |
dc.subject.INGV | 04. Solid Earth::04.04. Geology::04.04.01. Earthquake geology and paleoseismology | en_US |
dc.subject.INGV | 04. Solid Earth::04.04. Geology::04.04.04. Marine geology | en_US |
dc.subject.INGV | 04. Solid Earth::04.04. Geology::04.04.08. Sediments: dating, processes, transport | en_US |
dc.subject.INGV | 04. Solid Earth::04.04. Geology::04.04.09. Structural geology | en_US |
dc.subject.INGV | 04. Solid Earth::04.06. Seismology::04.06.05. Historical seismology | en_US |
dc.subject.INGV | 04. Solid Earth::04.07. Tectonophysics::04.07.07. Tectonics | en_US |
dc.identifier.doi | 10.1111/j.1365-3121.2009.00895.x | en_US |
dc.description.obiettivoSpecifico | 2T. Deformazione crostale attiva | en_US |
dc.description.journalType | JCR Journal | en_US |
dc.description.fulltext | open | en |
dc.contributor.author | Di Bucci, D. | - |
dc.contributor.author | Ridente, D. | - |
dc.contributor.author | Fracassi, U. | - |
dc.contributor.author | Trincardi, F. | - |
dc.contributor.author | Valensise, G. | - |
dc.contributor.department | P.C.M. - Dipartimento della Protezione Civile, 00189 Roma | en_US |
dc.contributor.department | Istituto di Geologia Ambientale e Geoingegneria, CNR, 00185 Roma | en_US |
dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italia | en_US |
dc.contributor.department | Istituto di Scienze Marine, CNR, 40129 Bologna | en_US |
dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italia | en_US |
item.openairetype | article | - |
item.cerifentitytype | Publications | - |
item.languageiso639-1 | en | - |
item.grantfulltext | open | - |
item.openairecristype | http://purl.org/coar/resource_type/c_18cf | - |
item.fulltext | With Fulltext | - |
crisitem.author.dept | Dipartimento della Protezione Civile | - |
crisitem.author.dept | Istituto di Geologia Ambientale e Geoingegneria, CNR, c/o Università Sapienza, P.le Aldo Moro 5, 00185 Rome (Italy) | - |
crisitem.author.dept | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia | - |
crisitem.author.dept | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia | - |
crisitem.author.orcid | 0000-0003-1290-4456 | - |
crisitem.author.orcid | 0000-0001-7102-514X | - |
crisitem.author.orcid | 0000-0001-7631-1903 | - |
crisitem.author.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
crisitem.author.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
crisitem.classification.parent | 04. Solid Earth | - |
crisitem.classification.parent | 04. Solid Earth | - |
crisitem.classification.parent | 04. Solid Earth | - |
crisitem.classification.parent | 04. Solid Earth | - |
crisitem.classification.parent | 04. Solid Earth | - |
crisitem.classification.parent | 04. Solid Earth | - |
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 | |
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Di Bucci et al., 2009_accettato.pdf | 2.43 MB | Adobe PDF | View/Open |
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