Surface faulting during the August 24, 2016, Central Italy earthquake (Mw 6.0): preliminary results
dc.contributor.author | Franz A. Livio, | |
dc.contributor.author | A. M. Michetti, | |
dc.contributor.author | E. Vittori, | |
dc.contributor.author | L. Gregory, | |
dc.contributor.author | L. Wedmore, | |
dc.contributor.author | L. Piccardi, | |
dc.contributor.author | E. Tondi, | |
dc.contributor.author | G. Roberts, | |
dc.contributor.author | CENTRAL ITALY EARTHQUAKE W.G., | |
dc.contributor.author | A. M. Blumetti, | |
dc.contributor.author | L. Bonadeo, | |
dc.contributor.author | F. Brunamonte, | |
dc.contributor.author | V. Comerci, | |
dc.contributor.author | P. Dimanna, | |
dc.contributor.author | M. F. Ferrario, | |
dc.contributor.author | J. Faure Walker, | |
dc.contributor.author | C. Frigerio, | |
dc.contributor.author | F. Fumanti, | |
dc.contributor.author | L. Guerrieri, | |
dc.contributor.author | F. Iezzi, | |
dc.contributor.author | G. Leoni, | |
dc.contributor.author | K. McCaffrey, | |
dc.contributor.author | Z. Mildon, | |
dc.contributor.author | R. Phillips, | |
dc.contributor.author | E. Rhodes, | |
dc.contributor.author | R. J. Walters, | |
dc.contributor.author | M. Wilkinson, | |
dc.date.accessioned | 2018-08-14T08:31:15Z | |
dc.date.available | 2018-08-14T08:31:15Z | |
dc.date.issued | 2016-11-24 | |
dc.identifier.issn | 1593-5213 | |
dc.identifier.issn | 2037-416X | |
dc.identifier.uri | http://hdl.handle.net/10026.1/12141 | |
dc.description.abstract |
We present some preliminary results on the mapping of coseismically-induced ground ruptures following the Aug. 24, 2016, Central Italy earthquake (Mw 6.0). The seismogenic source, as highlighted by InSAR and seismological data, ruptured across two adjacent structures: the Vettore and Laga faults. We collected field data on ground breaks along the whole deformed area and two different scenarios of on-fault coseismic displacement arise from these observations. To the north, along the Vettore fault, surface faulting can be mapped quite continuously along a well-defined fault strand while such features are almost absent to the south, along the Laga fault, where flysch-like marly units are present. A major lithological control, affects the surface expression of faulting, resulting in a complex deformation pattern. | |
dc.language.iso | en | |
dc.publisher | Instituto Nazionale di Geofisica e Vulcanologia, INGV | |
dc.title | Surface faulting during the August 24, 2016, Central Italy earthquake (Mw 6.0): preliminary results | |
dc.type | journal-article | |
dc.type | Journal Article | |
plymouth.author-url | https://www.webofscience.com/api/gateway?GWVersion=2&SrcApp=PARTNER_APP&SrcAuth=LinksAMR&KeyUT=WOS:000393514400011&DestLinkType=FullRecord&DestApp=ALL_WOS&UsrCustomerID=11bb513d99f797142bcfeffcc58ea008 | |
plymouth.issue | FASTTRACK5 | |
plymouth.volume | 59 | |
plymouth.publication-status | Published | |
plymouth.journal | Annals of Geophysics | |
dc.identifier.doi | 10.4401/ag-7197 | |
plymouth.organisational-group | /Plymouth | |
plymouth.organisational-group | /Plymouth/Faculty of Science and Engineering | |
plymouth.organisational-group | /Plymouth/Faculty of Science and Engineering/School of Geography, Earth and Environmental Sciences | |
plymouth.organisational-group | /Plymouth/REF 2021 Researchers by UoA | |
plymouth.organisational-group | /Plymouth/REF 2021 Researchers by UoA/UoA07 Earth Systems and Environmental Sciences | |
plymouth.organisational-group | /Plymouth/Users by role | |
plymouth.organisational-group | /Plymouth/Users by role/Academics | |
plymouth.organisational-group | /Plymouth/Users by role/Researchers in ResearchFish submission | |
dcterms.dateAccepted | 2016-08-24 | |
dc.rights.embargodate | 2023-6-21 | |
dc.identifier.eissn | 2037-416X | |
dc.rights.embargoperiod | Not known | |
rioxxterms.versionofrecord | 10.4401/ag-7197 | |
rioxxterms.licenseref.uri | http://www.rioxx.net/licenses/all-rights-reserved | |
rioxxterms.type | Journal Article/Review |