Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/8471
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dc.contributor.authorallStabile, T.; Istituto di Metodologie per l’Analisi Ambientale, CNR-IMAAen
dc.contributor.authorallIannaccone, G.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italiaen
dc.contributor.authorallZollo, A.; Dipartimento di Scienze Fisiche, Università di Napoli Federico II, Naplesen
dc.contributor.authorallLomax, A.; ALomax Scientific, Mouans-Sartoux, Franceen
dc.contributor.authorallFerulano, F.; ENI S.p.A. - E&P Division, San Donato Milanese (MI), Italyen
dc.contributor.authorallVetri, L.; ENI S.p.A. - E&P Division, San Donato Milanese (MI), Italyen
dc.contributor.authorallBarzaghi, L.; ENI S.p.A. - E&P Division, San Donato Milanese (MI), Italyen
dc.date.accessioned2012-12-20T08:28:57Zen
dc.date.available2012-12-20T08:28:57Zen
dc.date.issued2012en
dc.identifier.urihttp://hdl.handle.net/2122/8471en
dc.description.abstractThe accurate determination of locations and magnitudes of seismic events in a monitored region is important for many scientific, industrial and military studies and applications; for these purposes a wide variety of seismic networks are deployed throughout the world. It is crucial to know the performance of these networks not only in detecting and locating seismic events of different sizes throughout a specified source region, but also by evaluating their location errors as a function of the magnitude and source location. In this framework, we have developed a method for evaluating network performance in surface and borehole seismic monitoring. For a specified network geometry, station characteristics and a target monitoring volume, the method determines the lowest magnitude of events that the seismic network is able to detect (Mw detect), and locate (Mw loc) and estimates the expected location and origin time errors for a specified magnitude. Many of the features related to the seismic signal recorded at a single station are considered in this methodology, including characteristics of the seismic source, the instrument response, the ambient noise level, wave propagation in a layered, anelastic medium and uncertainties on waveform measures and the velocity model. We applied this method to two different network typologies: a local earthquake monitoring network, Irpinia Seismic Network (ISNet), installed along the Campania-Lucania Apennine chain in Southern Italy, and a hypothetic borehole network for monitoring microfractures induced during the hydrocarbon extraction process in an oil field. The method we present may be used to aid in enhancing existing networks and/or understanding their capabilities, such as for the ISNet case study, or to optimally design the network geometry in specific target regions, as for the borehole network example.en
dc.language.isoEnglishen
dc.publisher.nameWiley-Blackwellen
dc.relation.ispartofGeophysical Journal Internationalen
dc.relation.ispartofseries/192(2013)en
dc.subjectEarthquake ground motionsen
dc.subjectComputational seismologyen
dc.titleA comprehensive approach for evaluating network performance in surface and borehole seismic monitoringen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber793-806en
dc.subject.INGV04. Solid Earth::04.06. Seismology::04.06.10. Instruments and techniquesen
dc.identifier.doi10.1093/gji/ggs049en
dc.description.obiettivoSpecifico4.1. Metodologie sismologiche per l'ingegneria sismicaen
dc.description.journalTypeJCR Journalen
dc.description.fulltextrestricteden
dc.relation.issn0956-540Xen
dc.relation.eissn1365-246Xen
dc.contributor.authorStabile, T.en
dc.contributor.authorIannaccone, G.en
dc.contributor.authorZollo, A.en
dc.contributor.authorLomax, A.en
dc.contributor.authorFerulano, F.en
dc.contributor.authorVetri, L.en
dc.contributor.authorBarzaghi, L.en
dc.contributor.departmentIstituto di Metodologie per l’Analisi Ambientale, CNR-IMAAen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italiaen
dc.contributor.departmentDipartimento di Scienze Fisiche, Università di Napoli Federico II, Naplesen
dc.contributor.departmentENI S.p.A. - E&P Division, San Donato Milanese (MI), Italyen
dc.contributor.departmentENI S.p.A. - E&P Division, San Donato Milanese (MI), Italyen
dc.contributor.departmentENI S.p.A. - E&P Division, San Donato Milanese (MI), Italyen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextrestricted-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptUnivesità di Napoli, Federico II, Dip. Scienze Fisiche-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OV, Napoli, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OV, Napoli, Italia-
crisitem.author.deptENI S.p.A. - E&P Division, San Donato Milanese (MI), Italy-
crisitem.author.deptENI S.p.A. - E&P Division, San Donato Milanese (MI), Italy-
crisitem.author.deptENI S.p.A. - E&P Division, San Donato Milanese (MI), Italy-
crisitem.author.orcid0000-0002-1323-9016-
crisitem.author.orcid0000-0002-8191-9566-
crisitem.author.orcid0000-0002-7747-5990-
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-
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