Please use this identifier to cite or link to this item:
http://hdl.handle.net/2122/9273
DC Field | Value | Language |
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dc.contributor.authorall | Sandron, D.; OGS, Istituto Nazionale di Oceanografia e Geofisica Sperimentale, 34010 Sgonico (Trieste), Italy | en |
dc.contributor.authorall | Loreto, M. F.; ISMAR-CNR U.O.S. Bologna, Via Gobetti 101, 40129 Bologna, Italy | en |
dc.contributor.authorall | Fracassi, U.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italia | en |
dc.contributor.authorall | Tiberi, L.; Dipartimento di Matematica e Geoscienze, Università degli studi di Trieste, Via Weiss 4, 34129 Trieste, Italy | en |
dc.date.accessioned | 2015-01-19T14:49:31Z | en |
dc.date.available | 2015-01-19T14:49:31Z | en |
dc.date.issued | 2015 | en |
dc.identifier.uri | http://hdl.handle.net/2122/9273 | en |
dc.description.abstract | The destructive earthquake (M 7) that struck western Calabria (southern Italy) on 8 September 1905 profoundly hit a broad region, also generating a feeble tsunami. For all the damage it caused, this event was as much studied as not fully explained. Literature source models are numerous and diverse, in fault geometry, location, and associated magnitude. They also differ in nature, since these solutions are either field- based, or deriving from tsunami modeling, and macroseismic data inversion. Most. Neither all of these literature source models are not consistent with the damage pattern caused by the 1905 earthquake. To contribute to the identification of the seismogenic source of this destructive event, we performed a series of ground shaking scenarios, based on different faults that various authors associated with this event. The only documented data available suitable for our comparative purposes are the macroseismic intensities associated with localities affected by the event. We transformed the values of ground motion we computed for the same datapoints into intensities. We then attributed a quantitative fit to each modeled seismogenic source, evaluated with the quadratic sum of residuals between observed and calculated intensities. Our results show that two out of 7 literature source models are compatible with the damage distribution caused by the 1905 earthquake. The different parameters and boundary conditions constraining these two solutions suggest that either seismogenic source should include further complexities. Alternatively, since these two sources are antithetic and partially form a graben, they might have kinematically interacted, if passively, on 8 September 1905. | en |
dc.description.sponsorship | Project ISTEGE: “Indagine Sismotettonica del TErremoto dell'8 Settembre 1905 (Mw 7.4) nel Golfo di Sant'Eufemia – offshore tirrenico calabrese”, supported by OGS (Istituto Nazionale di Oceanografia e di Geofisica Sperimentale); Project RITMARE, funded by Dipartimento della Protezione Civile (Italy's National Civil Protection). | en |
dc.language.iso | English | en |
dc.publisher.name | Seismological Society of America | en |
dc.relation.ispartof | Bulletin of the Seismological Society of America | en |
dc.relation.ispartofseries | 2A/105 (2015) | en |
dc.subject | Shaking scenarios | en |
dc.subject | Seismogenic sources | en |
dc.subject | 1905 earthquake | en |
dc.subject | Southern Italy | en |
dc.title | Shaking scenarios from multiple source models shed light on the Mw 7 Calabria 8 September 1905 earthquake (S Italy) | en |
dc.type | article | en |
dc.description.status | Published | en |
dc.type.QualityControl | Peer-reviewed | en |
dc.description.pagenumber | 912-927 | en |
dc.subject.INGV | 04. Solid Earth::04.06. Seismology::04.06.03. Earthquake source and dynamics | en |
dc.subject.INGV | 04. Solid Earth::04.06. Seismology::04.06.04. Ground motion | en |
dc.subject.INGV | 04. Solid Earth::04.06. Seismology::04.06.11. Seismic risk | en |
dc.subject.INGV | 05. General::05.01. Computational geophysics::05.01.04. Statistical analysis | en |
dc.identifier.doi | 10.1785/0120140044 | en |
dc.description.obiettivoSpecifico | 3T. Pericolosità sismica e contributo alla definizione del rischio | en |
dc.description.journalType | JCR Journal | en |
dc.description.fulltext | reserved | en |
dc.relation.issn | 0037-1106 | en |
dc.relation.eissn | 1943-3573 | en |
dc.contributor.author | Sandron, D. | en |
dc.contributor.author | Loreto, M. F. | en |
dc.contributor.author | Fracassi, U. | en |
dc.contributor.author | Tiberi, L. | en |
dc.contributor.department | OGS, Istituto Nazionale di Oceanografia e Geofisica Sperimentale, 34010 Sgonico (Trieste), Italy | en |
dc.contributor.department | ISMAR-CNR U.O.S. Bologna, Via Gobetti 101, 40129 Bologna, Italy | en |
dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italia | en |
dc.contributor.department | Dipartimento di Matematica e Geoscienze, Università degli studi di Trieste, Via Weiss 4, 34129 Trieste, Italy | en |
item.openairetype | article | - |
item.cerifentitytype | Publications | - |
item.languageiso639-1 | en | - |
item.grantfulltext | reserved | - |
item.openairecristype | http://purl.org/coar/resource_type/c_18cf | - |
item.fulltext | With Fulltext | - |
crisitem.author.dept | Istituto Nazionale di Oceanografia e di Geofisica Sperimentale, Borgo Grotta Gigante 42/c, 34010 Sgonico (TS), Italy | - |
crisitem.author.dept | Istituto di Scienze Marine – Consiglio Nazionale delle Ricerche, Bologna, Italy | - |
crisitem.author.dept | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia | - |
crisitem.author.dept | Dipartimento di Matematica e Geoscienze, Università degli studi di Trieste, Via Weiss 4, 34129 Trieste, Italy | - |
crisitem.author.orcid | 0000-0003-1960-8684 | - |
crisitem.author.orcid | 0000-0001-7102-514X | - |
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 | 05. General | - |
crisitem.department.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
Appears in Collections: | Article published / in press |
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BSSA-Sandron_accepted.pdf | Accepted manuscript | 4.24 MB | Adobe PDF |
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