Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/10480
DC FieldValueLanguage
dc.contributor.authorallGarcía, L.en
dc.contributor.authorallÁlvarez, I.en
dc.contributor.authorallBenitez, C.en
dc.contributor.authorallTitos, M.en
dc.contributor.authorallBueno, A.en
dc.contributor.authorallMota, S.en
dc.contributor.authorallDe La Torre, A.en
dc.contributor.authorallSegura, J. C.en
dc.contributor.authorallAguacil, G.en
dc.contributor.authorallDiaz-Moreno, A.en
dc.contributor.authorallPrudencio, J.en
dc.contributor.authorallGarcia-Yeguas, A.en
dc.contributor.authorallIbanez, J. M.en
dc.contributor.authorallZuccarello, L.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Catania, Catania, Italiaen
dc.contributor.authorallCocina, O.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Catania, Catania, Italiaen
dc.contributor.authorallPatane, D.en
dc.date.accessioned2017-03-22T09:03:51Zen
dc.date.available2017-03-22T09:03:51Zen
dc.date.issued2016en
dc.identifier.urihttp://hdl.handle.net/2122/10480en
dc.description.abstractThis work describes the automatic picking of the P-phase arrivals of the 3*10^6 seismic registers originated during the TOMO-ETNA experiment. Air-gun shots produced by the vessel “Sarmiento de Gamboa” and contemporary passive seismicity occurring in the island are recorded by a dense network of stations deployed for the experiment. In such scenario, automatic processing is needed given: (i) the enormous amount of data, (ii) the low signal-to-noise ratio of many of the available registers and, (iii) the accuracy needed for the velocity tomography resulting from the experiment. A preliminary processing is performed with the records obtained from all stations. Raw data formats from the different types of stations are unified, eliminating defective records and reducing noise through filtering in the band of interest for the phase picking. The advanced multiband picking algorithm (AMPA) is then used to process the big database obtained and determine the travel times of the seismic phases. The approach of AMPA, based on frequency multiband denoising and enhancement of expected arrivals through optimum detectors, is detailed together with its calibration and quality assessment procedure. Examples of its usage for active and passive seismic events are presented.en
dc.language.isoEnglishen
dc.relation.ispartofANNALS OF GEOPHYSICSen
dc.relation.ispartofseries/59 (2016)en
dc.subjectMultiband frequency analysisen
dc.subjectAutomatic P-phase pickingen
dc.subjectActive/passive seismic phasesen
dc.subjectTOMO-ETNAen
dc.titleAdvances on the automatic estimation of the P-wave onset time.en
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumberS0434en
dc.subject.INGV04. Solid Earth::04.06. Seismology::04.06.09. Waves and wave analysisen
dc.identifier.doi10.4401/ag-7087en
dc.description.obiettivoSpecifico2V. Dinamiche di unrest e scenari pre-eruttivien
dc.description.journalTypeJCR Journalen
dc.description.fulltextopenen
dc.relation.eissn2037-416Xen
dc.contributor.authorGarcía, L.en
dc.contributor.authorÁlvarez, I.en
dc.contributor.authorBenitez, C.en
dc.contributor.authorTitos, M.en
dc.contributor.authorBueno, A.en
dc.contributor.authorMota, S.en
dc.contributor.authorDe La Torre, A.en
dc.contributor.authorSegura, J. C.en
dc.contributor.authorAguacil, G.en
dc.contributor.authorDiaz-Moreno, A.en
dc.contributor.authorPrudencio, J.en
dc.contributor.authorGarcia-Yeguas, A.en
dc.contributor.authorIbanez, J. M.en
dc.contributor.authorZuccarello, L.en
dc.contributor.authorCocina, O.en
dc.contributor.authorPatane, D.en
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Catania, Catania, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Catania, Catania, Italiaen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextopen-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptUniversidad de Granada, Departamento de Teoría de la Señal Telemática y Comunicaciones, Granada, Spain-
crisitem.author.deptDepartment of Signal Theory, Telematics and Communications, University of Granada, Spagna-
crisitem.author.deptUniversity of Granada, Spain-
crisitem.author.deptUniversity of Liverpool, UK-
crisitem.author.deptInstituto Andaluz de Geofisica, Universidad de Granada-
crisitem.author.deptInstituto Andaluz de Geofísica, Universidad de Granada, Granada, Spain-
crisitem.author.deptInstituto Andaluz de Geofísica, University of Granada, Granada, Spain,-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia, Sezione di Pisa, Italy-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia-
crisitem.author.orcid0000-0002-8279-2341-
crisitem.author.orcid0000-0002-9736-5190-
crisitem.author.orcid0000-0003-1755-3771-
crisitem.author.orcid0000-0002-9846-8781-
crisitem.author.orcid0000-0003-0094-9577-
crisitem.author.orcid0000-0003-1856-830X-
crisitem.author.orcid0000-0001-9410-5126-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent04. Solid Earth-
Appears in Collections:Article published / in press
Files in This Item:
File Description SizeFormat
Garcia_Zuccarello_AnnalsOfGeophysics_2016.pdfMain Article5.83 MBAdobe PDFView/Open
Show simple item record

WEB OF SCIENCETM
Citations 50

11
checked on Feb 10, 2021

Page view(s)

241
checked on Apr 20, 2024

Download(s) 20

438
checked on Apr 20, 2024

Google ScholarTM

Check

Altmetric