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Global and along-strike variations of source duration and scaling for intermediate-depth and deep-focus earthquakes

dc.creatorPrieto Gomez, German Andresspa
dc.creatorPoli, Pierospa
dc.date.accessioned2020-08-06T16:20:05Z
dc.date.available2020-08-06T16:20:05Z
dc.date.created2014-11-26spa
dc.description.abstractThe systematic behavior of earthquake rupture as a function of earthquake magnitude and/or tectonic setting is a key in our understanding of the physical mechanisms involved during earthquake rupture. Geophysical evidence suggests that although deep earthquakes—including intermediate?depth and deep—are similar to shallow ones, the mechanism involved during deep earthquakes is different from that of shallow ones. In particular, the magnitude and depth dependence of scaled duration, a measure of earthquake rupture duration, has led to controversy of what controls deep earthquake behavior. Here we estimate scaled source durations for 600 intermediate?depth and deep?focus earthquakes recorded at teleseismic distances and show deviation from self?similar scaling. No depth dependence is observed which we interpret as due to little differences between intermediate?depth and deep?focus earthquake mechanisms. The data show no correlation between durations and plate age or thermal parameters, suggesting that the thermal properties of the plate have little effect on source durations. We nevertheless report differences in average source duration and scaling between subduction zones and along?strike variations of source durations that more closely resemble the geometry of subduction (flat or steep subduction) rather than plate age.eng
dc.format.mimetypeapplication/pdf
dc.identifier.doihttps://doi.org/10.1002/2014GL061916
dc.identifier.issnISSN: 0094-8276
dc.identifier.issnESSN: 1944-8007
dc.identifier.urihttps://repository.urosario.edu.co/handle/10336/25872
dc.language.isoengspa
dc.publisherJohn Wiley and Sonsspa
dc.relation.citationEndPage8324
dc.relation.citationIssueNo. 23
dc.relation.citationStartPage8315
dc.relation.citationTitleGeophysical Research Letters
dc.relation.citationVolumeVol. 41
dc.relation.ispartofGeophysical Research Letters, ISSN: 0094-8276; ESSN: 1944-8007, Vol.41, No.23 (16 Diciembre, 2014); pp.8315-8324spa
dc.relation.urihttps://agupubs.onlinelibrary.wiley.com/doi/full/10.1002/2014GL061916spa
dc.rights.accesRightsinfo:eu-repo/semantics/openAccess
dc.rights.accesoAbierto (Texto Completo)spa
dc.sourceGeophysical Research Lettersspa
dc.source.instnameinstname:Universidad del Rosario
dc.source.reponamereponame:Repositorio Institucional EdocUR
dc.subject.keywordDeep?focus earthquakesspa
dc.subject.keywordRupture durationspa
dc.subject.keywordEarthquake scalingspa
dc.subject.keywordIntermediate?depth earthquakesspa
dc.subject.keywordSource time functionspa
dc.titleGlobal and along-strike variations of source duration and scaling for intermediate-depth and deep-focus earthquakesspa
dc.title.TranslatedTitleVariaciones globales y de largo alcance de duración de la fuente y escala para terremotos de profundidad intermedia y foco profundospa
dc.typearticleeng
dc.type.hasVersioninfo:eu-repo/semantics/publishedVersion
dc.type.spaArtículospa
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