Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/12820
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dc.date.accessioned2019-10-17T12:46:06Zen
dc.date.available2019-10-17T12:46:06Zen
dc.date.issued2004-01-17en
dc.identifier.urihttp://hdl.handle.net/2122/12820en
dc.descriptionBy studying the seismicity of the last 13 years in a region of central Italy, we have shown how the a and b parameters of the frequency-magnitude distribution change significantly in space and time, at short scale, especially in relation to an important seismic sequence. The b values were anomalously low especially in the Sellano area; indicating an anomalously large average magnitude in the regions later hit by the Sellano and Gualdo Tadino earthquakes.en
dc.description.abstractNearby faults can interact, affecting the timing of a future earthquake.Alarge earthquake can alter the static stress surrounding faults, possibly activating an aftershock sequence. Here we test the hypothesis of earthquake triggering by examining the earthquakes that affected the Umbria-Marche region (central Italy) during September 1997 to April 1998. The analysis was performed combining information contained in parameters a and b of the Gutenberg-Richter relationship, before and after the strongest main shocks, using a catalog of 6211 earthquakes (M 1.5). By analyzing the changes in space of the a parameter,we found that Colfiorito main shocks (Mw 5.7 and 6.0) on 26 September 1997 increased the seismicity rate within 40–50 km of the epicenter. We interpret this behavior as the effect of stress redistribution. After analyzing the b value changes in space and time we found the strongest increase in mean magnitude in the Sellano area, between the Colfiorito shocks and the two strong events (Mw 5.2 and 5.6, respectively) which hit this region on 12 and 14 October 1997. This area was also the location of the strongest increase in change of the local occurrence rate density. On the basis of these observations, we postulate that temporal variations in both a and b values indicate a probable causal connection between the largest earthquakes in the sequence.en
dc.language.isoEnglishen
dc.relation.ispartofJournal of geophysical research - solid earthen
dc.relation.ispartofseries/1019 (2004)en
dc.subjectb value, density rate change, earthquake triggeringen
dc.titleSeismicity and mean magnitude variations correlated to the strongest earthquakes of the 1997 Umbria-Marche sequence (central Italy)en
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumberB01304en
dc.subject.INGVSeismicity variations correlated to the strongest events of the 1997 Colfiorito sequenceen
dc.identifier.doi10.1029/2002JB002276en
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dc.description.obiettivoSpecifico6T. Studi di pericolosità sismica e da maremotoen
dc.description.journalTypeJCR Journalen
dc.contributor.authorMurru, Mauraen
dc.contributor.authorConsole, Rodolfoen
dc.contributor.authorLisi, Ariannaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italiaen
item.openairetypearticle-
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item.languageiso639-1en-
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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 Roma2, Roma, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia-
crisitem.author.orcid0000-0002-7385-394X-
crisitem.author.orcid0000-0002-7194-9489-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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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