Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/6112
DC FieldValueLanguage
dc.contributor.authorallDi Giulio, G.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.authorallSavvaidis, A.; ITSAK, Greeceen
dc.contributor.authorallTheodoulidis, N; ITSAK, Greeceen
dc.contributor.authorallOhrnberger, M.; University of Potsdam, Germanyen
dc.contributor.authorallEndrun, B.; University of Potsdam, Germanyen
dc.contributor.authorallWathelet, M.; LGIT, Grenoble, Franceen
dc.contributor.authorallCornou, C.; LGIT, Grenoble, Franceen
dc.contributor.authorallRenalier, F.; LGIT, Grenoble, Franceen
dc.contributor.authorallBard, P.; LGIT, Grenoble, Franceen
dc.date.accessioned2010-09-13T09:12:17Zen
dc.date.available2010-09-13T09:12:17Zen
dc.date.issued2010en
dc.identifier.urihttp://hdl.handle.net/2122/6112en
dc.description.abstractWithin the scope of the EC-projects NERIES and ITSAK-GR we have applied a procedure able to combine a multi-model space parameterization and an information theoretic approach in analysis of dispersion curve inversion. In detail we considered the dispersion curve assessed at 14 strong motion European sites. At each site we investigated the model space through four different parameterization groups within the wavelength range estimated by actual dispersion curves. In order to explore the influence of model space we increased progressively the number of layers for each parameterization. We therefore addressed the model evaluation among a set of competing models obtained by inversion following the corrected Akaike’s Information Criterion(AICc). By using such information-theoretic approach, we found an acceptable agreement between the inverted shear-velocity profiles of the best models and the available borehole results.en
dc.description.sponsorshipIZIISen
dc.language.isoEnglishen
dc.relation.ispartof14th ECEEen
dc.subjectsurface waves, inversion of dispersion curves, Akaike's information criterionen
dc.titleInversion of surface wave dispersion at european strong motion sites using a multi-model parameterization and an information-theoretic approachen
dc.typeExtended abstracten
dc.description.statusPublisheden
dc.subject.INGV04. Solid Earth::04.02. Exploration geophysics::04.02.99. General or miscellaneousen
dc.description.ConferenceLocationOhrid, Republic of Macedoniaen
dc.relation.referencesAkaike, H. (1974). A new look at the statistical model identification. IEEE Trans. Automat. Contr. 19, 716-723. Aki, K. (1957). Space and time spectra of stationary stochastic waves, with special reference to microtremors. Bull. Earth. Res. Inst. Tokyo Univ. 25, 415-457. Asten, M. W., Dhu, T., and Lam, N. (2004). Optimized array design for microtremor array studies applied to site classification; comparison of results with SCPT logs. In Proc. of 13th World Conf. on Earthquake Engineering, paper no. 2903, Vancouver, B.C., Canada. Bettig, B., Bard, P.-Y., Scherbaum, F., Riepl, J., Cotton, F., Cornou, C., and Hatzfeld, D. (2001). Analysis of dense array noise measurements using the modified spatial auto-correlation method (SPAC). Application to the Grenoble area., Boll. Geof. Teor. Appl. 42, 281–304. Bozdogan, H. (2000). Akaike’s Information Criterion and Recent Developments in Information Complexity, Journal of Mathematical Psychology 44, 62–91. Burham, K.P. and Anderson, D.R. (2001). Kullback-Leibler information as a basis for strong inference in ecological studies. Wildlife Research 28, 111-119. Capon, J. (1969). High-resolution frequency–wavenumber spectrum analysis, Proc. IEEE 57:8, 1408–1418. Di Giulio, G., Cornou, C., Ohrnberger, M., Wathelet, M. and Rovelli, A. (2006). Deriving wavefield characteristics and shear-velocity profiles from two-dimensional small-aperture arrays analysis of ambient vibrations in a small-size alluvial basin, Colfiorito, Italy. Bull. Seism. Soc. Am. 96:5, 1915-1933. Endrun, B., Ohrnberger, M. and Savvaidis, A. (2009). On the repeatability and consistency of three-component ambient vibration array measurements, Bull. Earthquake Eng., doi 10.1007/s10518-009-9159-9. Kohler, A., Ohrnberger, M., Scherbaum, F., Wathelet, M. and Cornou, C. (2007). Assessing the reliability of the modified three-component spatial autocorrelation technique, Geophys. J. Int. 168, 779–796. Kullback, S. and Leibler, R. (1951). On information and sufficiency, Annals of Mathematical Statistics 22, 79-86. Lacoss, R.T., Kelly, E.J. and Toksöz, M.N. (1969). Estimation of seismic noise structure using arrays.Geophysics 34, 21–38. Park, C. B., Miller, R. D. and Xia, J. (1999). Multi-channel analysis of surface waves (MASW), Geophysics 64, 800–808. Renalier, F. (2010). Caractérisation sismique de sites hétérogènes à partir de méthodes actives et passives: variations latérales et temporelles, Ph.D. Thesis, Joseph Fourier University, Grenoble, 224 pages. Sambridge, M. (1999). Geophysical inversion with a neighbourhood algorithm: I. Searching a parameter space, Geophys. J. Int. 138, 479– 494, doi:10.1046/j.1365-246X.1999.00876.x Savvaidis, A., Ohrnberger, M., Wathelet, M., Cornou, C., Bard, P.-Y. and Theodoulidis, N. (2009). Variability analysis of shallow shear wave velocity profiles obtained from dispersion curve inversion considering multiple model parameterization. Abstract in Seismological Research Letters 80:2, 354, SSA Meeting, April 2009, Monterey, USA. Wathelet, M., Jongmans, D. and Ohrnberger, M. (2005). Direct Inversion of Spatial Autocorrelation Curves with the Neighborhood Algorithm. Bull. Seism. Soc. Am. 95, 1787-1800. Wathelet, M., Jongmans, D., Ohrnberger, M. and Bonnefoy-Claudet, S. (2008). Array performance for ambient vibrations on a shallow structure and consequences over Vs inversion. J. Seism. 12, 1–19. doi:10.1007/s10950-007-9067-x Wathelet, M. (2008). An improved neighborhood algorithm: parameter conditions and dynamic scaling. Geophys. Res. Lett. 35, L09301, DOI:10.1029/2008GL033256en
dc.description.obiettivoSpecifico4.1. Metodologie sismologiche per l'ingegneria sismicaen
dc.description.fulltextopenen
dc.contributor.authorDi Giulio, G.en
dc.contributor.authorSavvaidis, A.en
dc.contributor.authorTheodoulidis, Nen
dc.contributor.authorOhrnberger, M.en
dc.contributor.authorEndrun, B.en
dc.contributor.authorWathelet, M.en
dc.contributor.authorCornou, C.en
dc.contributor.authorRenalier, F.en
dc.contributor.authorBard, P.en
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.departmentITSAK, Greeceen
dc.contributor.departmentITSAK, Greeceen
dc.contributor.departmentUniversity of Potsdam, Germanyen
dc.contributor.departmentUniversity of Potsdam, Germanyen
dc.contributor.departmentLGIT, Grenoble, Franceen
dc.contributor.departmentLGIT, Grenoble, Franceen
dc.contributor.departmentLGIT, Grenoble, Franceen
dc.contributor.departmentLGIT, Grenoble, Franceen
item.openairetypeExtended abstract-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextopen-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia-
crisitem.author.deptITSAK-
crisitem.author.deptITSAK, Thessaloniki, Grrece-
crisitem.author.deptIGUP, Potsam, Germany-
crisitem.author.deptUniversity of Potsdam, Germany-
crisitem.author.deptLGIT, University J. Fourier, Grenoble, France-
crisitem.author.deptUniversité Joseph Fourier, Institut des Sciences de la Terre, Grenoble, France-
crisitem.author.deptLGIT, Grenoble, France-
crisitem.author.orcid0000-0002-4097-7102-
crisitem.author.orcid0000-0002-0664-5315-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent04. Solid Earth-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
Appears in Collections:Conference materials
Files in This Item:
File Description SizeFormat
1434.pdfExtended conference paper667.1 kBAdobe PDFView/Open
Show simple item record

Page view(s)

165
checked on Apr 13, 2024

Download(s) 10

517
checked on Apr 13, 2024

Google ScholarTM

Check