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Earthquakes initiation and thermal shear instability in the Hindu Kush intermediate depth nest

dc.creatorPoli, Pierospa
dc.creatorPrieto, German A.
dc.creatorRivera, Efrainspa
dc.creatorRuiz, Sergiospa
dc.date.accessioned2020-08-06T16:20:05Z
dc.date.available2020-08-06T16:20:05Z
dc.date.created2016-02-04spa
dc.description.abstractIntermediate depth earthquakes often occur along subducting lithosphere, but despite their ubiquity the physical mechanism responsible for promoting brittle or brittle?like failure is not well constrained. Large concentrations of intermediate depth earthquakes have been found to be related to slab break?off, slab drip, and slab tears. The intermediate depth Hindu Kush nest is one of the most seismically active regions in the world and shows the correlation of a weak region associated with ongoing slab detachment process. Here we study relocated seismicity in the nest to constraint the geometry of the shear zone at the top of the detached slab. The analysis of the rupture process of the Mw 7.5 Afghanistan 2015 earthquake and other several well?recorded events over the past 25?years shows an initially slow, highly dissipative rupture, followed by a dramatic dynamic frictional stress reduction and corresponding large energy radiation. These properties are typical of thermal driven rupture processes. We infer that thermal shear instabilities are a leading mechanism for the generation of intermediated?depth earthquakes especially in presence of weak zone subjected to large strain accumulation, due to ongoing detachment process.eng
dc.format.mimetypeapplication/pdf
dc.identifier.doihttps://doi.org/10.1002/2015GL067529
dc.identifier.issnISSN: 0094-8276
dc.identifier.issnESSN: 1944-8007
dc.identifier.urihttps://repository.urosario.edu.co/handle/10336/25871
dc.language.isoengspa
dc.publisherJohn Wiley and Sonsspa
dc.relation.citationEndPage1542
dc.relation.citationIssueNo. 4
dc.relation.citationStartPage1537
dc.relation.citationTitleGeophysical Research Letters
dc.relation.citationVolumeVol. 43
dc.relation.ispartofGeophysical Research Letters, ISSN: 0094-8276; ESSN: 1944-8007, Vol.43, No.4 (Febrero, 2016); pp.1537-1542spa
dc.relation.urihttps://agupubs.onlinelibrary.wiley.com/doi/full/10.1002/2015GL067529spa
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 Earthquakesspa
dc.subject.keywordSubduction zonesspa
dc.subject.keywordEarthquake energy releasespa
dc.subject.keywordEarthquakes nestspa
dc.subject.keywordThermal shear instabilityspa
dc.subject.keywordSeismologyspa
dc.titleEarthquakes initiation and thermal shear instability in the Hindu Kush intermediate depth nestspa
dc.title.TranslatedTitleIniciación de terremotos e inestabilidad por cizallamiento térmico en el nido de profundidad intermedia Hindu Kushspa
dc.typearticleeng
dc.type.hasVersioninfo:eu-repo/semantics/publishedVersion
dc.type.spaArtículospa
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