Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/11719
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dc.date.accessioned2018-04-20T08:38:41Zen
dc.date.available2018-04-20T08:38:41Zen
dc.date.issued2017-06-06en
dc.identifier.urihttp://hdl.handle.net/2122/11719en
dc.description.abstractInduced seismicity associated with energy production is becoming an increasingly important issue worldwide for the hazard it poses to the exposed population and structures. We analyze one of the rare cases of induced seismicity associated with the underwater gas storage operations observed in the Castor platform, located in the Valencia gulf, east Spain, near a complex and important geological structure. In September 2013, some gas injection operations started at Castor, producing a series of seismic events around the reservoir area. The larger magnitude events (up to 4.2) took place some days after the end of the injection, with EMS intensities in coastal towns up to degree III. In this work, the seismic sequence is analyzed with the aim of detecting changes in statistical parameters describing the earthquake occurrence before and after the injection and identifying possible proxies to be used for monitoring the sequence evolution. Moreover, we explore the potential predictability of these statistical parameters which can be used to control the field operations in injection/storage fluid reservoirs. We firstly perform a retrospective approach and next a perspective analysis. We use different techniques for estimating the value of the expected maximum magnitude that can occur due to antropogenic activities in Castor.en
dc.language.isoEnglishen
dc.relation.ispartofScientific reportsen
dc.relation.ispartofseries/7 (2017)en
dc.titleTemporal evolution of a seismic sequence induced by a gas injection in the Eastern coast of Spainen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber2901en
dc.identifier.URLhttps://www.nature.com/articles/s41598-017-02773-2.pdfen
dc.subject.INGVInduced seismicityen
dc.identifier.doi10.1038/s41598-017-02773-2en
dc.description.obiettivoSpecifico2T. Sorgente Sismicaen
dc.description.journalTypeJCR Journalen
dc.relation.eissn2045-2322en
dc.contributor.authorRuiz Rosales, Santiagoen
dc.contributor.authorSharma, N.en
dc.contributor.authorConvertito, Vincenzoen
dc.contributor.authorZollo, Aldoen
dc.contributor.authorBenito, E.en
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OV, Napoli, Italiaen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextopen-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptDipartimento di Scienze Fisiche Università degli Studi di Napoli “Federico II”-
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.deptElectromagnetism and Radar Department, Onera, Palaiseau, France-
crisitem.author.orcid0000-0001-9536-3696-
crisitem.author.orcid0000-0002-7115-7502-
crisitem.author.orcid0000-0002-8191-9566-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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