Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/4172
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dc.contributor.authorallPignatelli, A.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italiaen
dc.contributor.authorallGiuntini, A.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italiaen
dc.contributor.authorallConsole, R.; Italian National Data Center, viale Pinturicchio 23/E, 00196 Roma, Italyen
dc.date.accessioned2008-11-18T15:25:33Zen
dc.date.available2008-11-18T15:25:33Zen
dc.date.issued2008-07en
dc.identifier.urihttp://hdl.handle.net/2122/4172en
dc.description.abstractWe develop and implement an algorithm for inverting three-element array data on a Matlab platform. The algorithm allows reliable estimation of back azimuth and apparent velocity from seismic records under low signal-to-noise conditions. We start with a cubic spline interpolation of the waveforms and determine the differences between arrival times at pairs of array elements. The time differences are directly computed from cross-correlation functions. The advantages of this technique are (a) manual picking of the onset of each arrival is not necessary at each array element; (b) interpolation makes it possible to estimate time differences at a higher resolution than the sampling rate of the digital waveforms; (c) consistency among three independent determinations provides a reliability check; and (d) the value of apparent velocity indicates the nature of the recorded wavelet and physically checks the results. The algorithm was tested on data collected by a tri-partite array (with an aperture of 250 m) deployed in 1998 by the National Data Center of Israel, during a field experiment in southern Israel, 20km southwest of the Dead Sea. The data include shallow explosions and natural earthquakes under both high and low signal-to-noise conditions. The procedure developed in this study is considered suitable for searching of small aftershocks subsequent to an underground explosion, in the context of on-site inspections according to the Comprehensive Nuclear-Test-Ban Treaty (CTBT).en
dc.language.isoEnglishen
dc.publisher.nameElsevier Ltd.en
dc.relation.ispartofComputers & Geosciencesen
dc.relation.ispartofseries7 / 34 (2008)en
dc.relation.isversionofhttp://hdl.handle.net/2122/3145en
dc.subjectCross-correlationen
dc.subjectLocationen
dc.subjectAutomationen
dc.subjectArray processingen
dc.subjectCTBTen
dc.titleMatlab software for the analysis of seismic waves recorded by three-element arraysen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber792-801en
dc.subject.INGV04. Solid Earth::04.02. Exploration geophysics::04.02.06. Seismic methodsen
dc.identifier.doi10.1016/j.cageo.2007.10.003en
dc.relation.referencesAdushkin, V., Spivak, A., 1995. Aftershocks of underground nuclear explosions. In: Console, R., Nikolaev, A. (Eds.), Earthquakes Induced by Underground Nuclear Explosions, NATO ASI Series, Partnership Sub-Series, 2. Environment, vol. 4. Springer, Berlin Heidelberg, pp. 21–34. Almendros, J., Ibanez, J.M., Alguacil, G., Del Pezzo, E., 1999. Array analysis using circular-wave-front geometry: an application to locate the nearby seismo-volcanic source. Geophysical Journal International 136, 159–170. Bartal, Y., Villagran, M., Ben Horin, Y., Leonard, G., Joswig, M., 2000. Definition of exclusive zones using seismic data. Pure and Applied Geophysics 158, 397–419. Richards, P.G., Ekstrom, G., 1995. Earthquake activity associated with underground nuclear explosions. In: Console, R., Nikolaev, A. (Eds.), Earthquakes Induced by Underground Nuclear Explosions, NATO ASI Series, Partnership Sub- Series, 2. Environment, vol. 4. Springer, Berlin, Heidelberg, pp. 35–49. Taylor, J.R., 1982. An Introduction to Error Analysis, the Study of Uncertainties in Physical Measurements. University Science Books, Sausalito, CA, 327 pp.en
dc.description.obiettivoSpecifico3.8. Geofisica per l'ambienteen
dc.description.journalTypeJCR Journalen
dc.description.fulltextpartially_openen
dc.contributor.authorPignatelli, A.en
dc.contributor.authorGiuntini, A.en
dc.contributor.authorConsole, R.en
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italiaen
dc.contributor.departmentItalian National Data Center, viale Pinturicchio 23/E, 00196 Roma, Italyen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextrestricted-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma2, Roma, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma2, Roma, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma2, Roma, Italia-
crisitem.author.orcid0000-0002-3172-2044-
crisitem.author.orcid0000-0002-0457-1033-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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-
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