Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/4589
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dc.contributor.authorallMayeda, K.; Weston Geophysical Corporation, Lexington, MAen
dc.contributor.authorallMalagnini, L.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.date.accessioned2008-12-11T09:28:25Zen
dc.date.available2008-12-11T09:28:25Zen
dc.date.issued2009-
dc.identifier.urihttp://hdl.handle.net/2122/4589en
dc.description.abstractApparent stress and corner frequencies are measured for the Chi-Chi, Taiwan sequence beginning with the Mw 7.6 mainshock on 20 September 1999. Using the coda source ratio method, we obtained stable source ratio estimates using broadband stations on Taiwan. We find the following: (1) For the mainshock and 3 of the larger aftershocks, apparent stress is clustered around 0.8 MPa (+/- 0.1 MPa); (2) Events below ~Mw 5.5 exhibit lower apparent stress with larger scatter, ranging between ~0.08 and 0.8 MPa and are spatially variable; 3) The Brune [1970, 1971] omega-square source model fits the spectral shape for events 4.7<Mw<7.6, however a step-wise break in self-similarity exists at ~Mw 5.5. We hypothesize that larger events are subject to the regional state-of-stress, whereas smaller aftershocks are sensitive to the local state-of-stress from stress-field redistribution following the mainshock and/or fault zone lubrication that affects only larger events.en_US
dc.language.isoEnglishen_US
dc.relation.ispartofGeophysical Research Lettersen_US
dc.relation.ispartofseries10/36 (2009)en_US
dc.subjectearthquake fault dynamicsen_US
dc.subjectapparent stressen_US
dc.subjectdynamic stress dropen_US
dc.titleApparent Stress and Corner Frequency Variations in the 1999 Taiwan (Chi-Chi) Sequence: Evidence For a Step-Wise Increase at Mw ~5.5en_US
dc.typearticleen_US
dc.description.statusPublisheden_US
dc.description.pagenumberL10308en_US
dc.subject.INGV04. Solid Earth::04.06. Seismology::04.06.03. Earthquake source and dynamicsen_US
dc.identifier.doi10.1029/2009GL037421en_US
dc.description.obiettivoSpecifico3T. Sorgente sismicaen_US
dc.description.journalTypeJCR Journalen_US
dc.description.fulltextreserveden
dc.contributor.authorMayeda, K.-
dc.contributor.authorMalagnini, L.-
dc.contributor.departmentWeston Geophysical Corporation, Lexington, MAen_US
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen_US
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextrestricted-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptUC Berkeley-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia-
crisitem.author.orcid0000-0003-0980-0605-
crisitem.author.orcid0000-0001-5809-9945-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent04. Solid Earth-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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