Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/1941
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dc.contributor.authorallBernard, P.; Département de Sismologie, I.P.G.P., Paris, Franceen
dc.contributor.authorallHerrero, A.; Département de Sismologie, I.P.G.P., Paris, Franceen
dc.date.accessioned2006-12-06T11:35:41Zen
dc.date.available2006-12-06T11:35:41Zen
dc.date.issued1994-12en
dc.identifier.urihttp://hdl.handle.net/2122/1941en
dc.description.abstractWe present a broadband kinematic model based on a self-similar k-square distribution of the coseismic slip, with an instantaneous rise-time and a constant rupture velocity. The phase of the slip spectrum at high wave number is random. This model generates an ?-squared body-wave radiation, and a particular directivity factor C2d scaling the amplitude of the body-wave spectra, where Cd is the standard directivity factor. Considering the source models with a propagating pulse and a finite rise-time, we assume that within the slipping band, the rupture has some random character, with small scale rupture in various directions. With such a model, the pulse cannot be resolved, and the directivity factor is still C2d at low frequency; at periods shorter than the rise-time, however, the directivity effect drops to much smaller rms values. This frequency dependent directivity effect, which is expected to be the strongest for sites located in the direction of rupture, was evidenced for the Landers 1992 earthquake, leading to a 2 to 3 s rise-time of the slip pulse. This kinematic model can be used with more refined theoretical Green's functions, including near-field terms and surface waves, or with empirical Green's functions, for generating realistic broadband records in the vicinity of moderate to large earthquakes, in a frequency range relevant for engineering applications (0 Hz to about 20 Hz).en
dc.format.extent3654957 bytesen
dc.format.mimetypeapplication/pdfen
dc.language.isoEnglishen
dc.relation.ispartofseries6/37 (1994)en
dc.subjectfault slipen
dc.subjectseismic ruptureen
dc.subjectslip heterogeneityen
dc.subjectdirectivity effecten
dc.subjectkinematic ruptureen
dc.subjectstochastic modelen
dc.titleSlip heterogeneity, body-wave spectra, and directivity of earthquake rupturesen
dc.typearticleen
dc.type.QualityControlPeer-revieweden
dc.subject.INGV04. Solid Earth::04.06. Seismology::04.06.99. General or miscellaneousen
dc.description.journalTypeJCR Journalen
dc.description.fulltextopenen
dc.contributor.authorBernard, P.en
dc.contributor.authorHerrero, A.en
dc.contributor.departmentDépartement de Sismologie, I.P.G.P., Paris, Franceen
dc.contributor.departmentDépartement de Sismologie, I.P.G.P., Paris, Franceen
item.languageiso639-1en-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.cerifentitytypePublications-
item.fulltextWith Fulltext-
item.openairetypearticle-
item.grantfulltextopen-
crisitem.author.deptInstitut de Physique du Globe de Paris, Dèpartement de Seismologie, Paris, France-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia-
crisitem.author.orcid0000-0001-5633-5852-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent04. Solid Earth-
Appears in Collections:Annals of Geophysics
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