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Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/3571
DC FieldValueLanguage
dc.contributor.authorallNielsen, S.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.editorallGasparini, P.en
dc.contributor.editorallManfredi, G.en
dc.contributor.editorallZschau, J.en
dc.date.accessioned2008-02-25T07:10:46Zen
dc.date.available2008-02-25T07:10:46Zen
dc.date.issued2007en
dc.identifier.isbn978-3-540-72240-3en
dc.identifier.urihttp://hdl.handle.net/2122/3571en
dc.description.abstractIt has been argued that the dominant period T_p derived from the initial seconds of a seismogram, hence only depending on the initial phases of earthquake rupture, seems to scale with the final size of the earthquake. We provide a physical interpretation for the observed scaling and explain how the final earthquake size could be controlled by the initial phase of rupture.en
dc.language.isoEnglishen
dc.publisher.nameSpringeren
dc.relation.ispartofEarthquake Early warning systemsen
dc.subjectearly warningen
dc.subjectfracture energyen
dc.titleCan earthquake size be controlled by the initial seconds of rupture?en
dc.typebook chapteren
dc.description.statusPublisheden
dc.type.QualityControlUnreferreden
dc.description.pagenumber9-19en
dc.subject.INGV04. Solid Earth::04.06. Seismology::04.06.03. Earthquake source and dynamicsen
dc.description.obiettivoSpecifico3.1. Fisica dei terremotien
dc.description.fulltextreserveden
dc.contributor.authorNielsen, S.en
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.editorGasparini, P.en
dc.contributor.editorManfredi, G.en
dc.contributor.editorZschau, J.en
item.openairetypebook chapter-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextrestricted-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptDurham University, Durham, UK-
crisitem.author.orcid0000-0002-9214-2932-
crisitem.classification.parent04. Solid Earth-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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