Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/6398
DC FieldValueLanguage
dc.contributor.authorallOglesby, D.; University of California, Riversideen
dc.contributor.authorallArchuleta, R.; Institure for crustal studies, university of santa barbara, californiaen
dc.contributor.authorallNielsen, S.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.date.accessioned2010-12-16T10:56:53Zen
dc.date.available2010-12-16T10:56:53Zen
dc.date.issued1998en
dc.identifier.urihttp://hdl.handle.net/2122/6398en
dc.description.abstractDynamic simulations of earthquakes on dipping faults show asymmetric near-source ground motion caused by the asymmetric geometry of such faults. The ground motion from a thrust or reverse fault is larger than that of a normal fault by a factor of 2 or more, given identical initial stress magnitudes. The motion of the hanging wall is larger than that of the footwall in both thrust (reverse) and normal earthquakes. The asymmetry between normal and thrust (reverse) faults results from time-dependent normal stress caused by the interaction of the earthquake-generated stress field with Earth’s free surface. The asymmetry between hanging wall and footwall results from the asymmetric mass and geometry on the two sides of the fault.en
dc.language.isoEnglishen
dc.publisher.nameSCIENCEen
dc.relation.ispartofSCIENCEen
dc.relation.ispartofseries/280 (1998)en
dc.subjectfoot wallen
dc.subjecthanging wallen
dc.titleEarthquakes on dipping faults: the effects of broken symmetryen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber1055-1059en
dc.subject.INGV04. Solid Earth::04.06. Seismology::04.06.03. Earthquake source and dynamicsen
dc.description.obiettivoSpecifico3.1. Fisica dei terremotien
dc.description.journalTypeJCR Journalen
dc.description.fulltextreserveden
dc.contributor.authorOglesby, D.en
dc.contributor.authorArchuleta, R.en
dc.contributor.authorNielsen, S.en
dc.contributor.departmentUniversity of California, Riversideen
dc.contributor.departmentInstiture for crustal studies, university of santa barbara, californiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
item.languageiso639-1en-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
item.cerifentitytypePublications-
item.openairetypearticle-
item.grantfulltextrestricted-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent04. Solid Earth-
crisitem.author.deptUniversity of California, Riverside-
crisitem.author.deptInstitute for Crustal Studies, University of California, Santa Barbara, CA. U.S.A.-
crisitem.author.deptDurham University, Durham, UK-
crisitem.author.orcid0000-0002-9214-2932-
Appears in Collections:Article published / in press
Files in This Item:
File Description SizeFormat Existing users please Login
Oglesby1998_Science.pdf398.35 kBAdobe PDF
Show simple item record

Page view(s)

85
checked on Sep 25, 2022

Download(s)

20
checked on Sep 25, 2022

Google ScholarTM

Check