Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/7556
DC FieldValueLanguage
dc.contributor.authorallSchubnel, A.; ENS Paris, UMR8538, CNRS, Geol Lab, Paris, Franceen
dc.contributor.authorallNielsen, S.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.authorallTaddeucci, J.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.authorallVinciguerra, S.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.authorallRao, S.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.date.accessioned2012-01-26T07:28:06Zen
dc.date.available2012-01-26T07:28:06Zen
dc.date.issued2011-08-15en
dc.identifier.urihttp://hdl.handle.net/2122/7556en
dc.description.abstractWe report supershear ruptures observed in spontaneously nucleating laboratory microearthquakes and describe the signature of the associated Mach wavefront radiation. Transducers detect the wavefield both close and at a distance from the fault. The rupture velocities are inferred from either photoelastic high-speed imaging or using the acoustic recordings; both methods yield compatible estimates of sufficient accuracy to discriminate between sub-shear and supershear ruptures. The acoustic records allow to characterize the Mach wavefront radiated from the supershear rupture front, in particular its amplitude and decay. Velocity functions recovered by integrating high frequency accelerometer signals in the case of supershear ruptures, consist in a double-pulse function: a first pulse traveling at supershear velocity followed by a second pulse traveling at the Rayleigh wave velocity. Conversely, the sub-shear event is characterized by a single pulse. Finally, we perform numerical simulations of our experiment using a prescribed supershear rupture velocity. The synthetic waveforms obtained from these simulations, including the Mach wave amplitude and phase, yield a satisfactory fit to the experimental results. (C) 2011 Elsevier B.V. All rights reserved.en
dc.description.sponsorshipEuropean Research Council (USEMS), AMRA, TRIGSen
dc.language.isoEnglishen
dc.publisher.nameElsevieren
dc.relation.ispartofEarth and Planetary Science Lettersen
dc.relation.ispartofseries3-4/308 (2011)en
dc.subjectanalog modelsen
dc.subjectdynamic fractureen
dc.subjectphotoelasticityen
dc.subjectacoustic emissionen
dc.titlePhoto-acoustic study of subshear and supershear ruptures in the laboratoryen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber424–432en
dc.subject.INGV04. Solid Earth::04.04. Geology::04.04.06. Rheology, friction, and structure of fault zonesen
dc.identifier.doi10.1016/j.epsl.2011.06.013en
dc.description.obiettivoSpecifico3.1. Fisica dei terremotien
dc.description.journalTypeJCR Journalen
dc.description.fulltextreserveden
dc.contributor.authorSchubnel, A.en
dc.contributor.authorNielsen, S.en
dc.contributor.authorTaddeucci, J.en
dc.contributor.authorVinciguerra, S.en
dc.contributor.authorRao, S.en
dc.contributor.departmentENS Paris, UMR8538, CNRS, Geol Lab, Paris, Franceen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextrestricted-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptENS, France-
crisitem.author.deptDurham University, Durham, UK-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia-
crisitem.author.orcid0000-0002-9214-2932-
crisitem.author.orcid0000-0002-0516-3699-
crisitem.author.orcid0000-0002-6939-3549-
crisitem.author.orcid0000-0001-7934-4786-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent04. Solid Earth-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
Appears in Collections:Article published / in press
Files in This Item:
File Description SizeFormat Existing users please Login
SchubnelEPSL2011.pdfmain paper1.52 MBAdobe PDF
Show simple item record

WEB OF SCIENCETM
Citations 20

25
checked on Feb 10, 2021

Page view(s)

197
checked on Apr 24, 2024

Download(s)

19
checked on Apr 24, 2024

Google ScholarTM

Check

Altmetric