Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/10870
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dc.contributor.authorallChiaraluce, Lauro; Istituto Nazionale di Geofisica e Vulcanologia, Sezione CNT, Roma, Italiaen
dc.contributor.authorallCollettini, Cristianoen
dc.contributor.authorallCattaneo, Marco; Istituto Nazionale di Geofisica e Vulcanologia, Sezione CNT, Roma, Italiaen
dc.contributor.authorallMonachesi, Giancarlo; Istituto Nazionale di Geofisica e Vulcanologia, Sezione CNT, Roma, Italiaen
dc.date.accessioned2018-02-28T09:45:54Zen
dc.date.available2018-02-28T09:45:54Zen
dc.date.issued2014en
dc.identifier.urihttp://hdl.handle.net/2122/10870en
dc.description.abstractAs part of an interdisciplinary research project, funded by the European Research Council and addressing the mechanics of weak faults, we drilled three 200–250 m-deep boreholes and installed an array of seismometers. The array augments TABOO (The AltotiBerina near fault ObservatOry), a scientific infrastructure managed by the Italian National Institute of Geophysics and Volcanology. The observatory, which consists of a geophysical network equipped with multi-sensor stations, is located in the northern Apennines (Italy) and monitors a large and active low-angle normal fault. The drilling operations started at the end of 2011 and were completed by July 2012. We instrumented the boreholes with three-component short-period (2 Hz) passive instruments at different depths. The seismometers are now fully operational and collecting waveforms characterised by a very high signal to noise ratio that is ideal for studying microearthquakes. The resulting increase in the detection capability of the seismic network will allow for a broader range of transients to be identified.en
dc.language.isoEnglishen
dc.relation.ispartofSCIENTIFIC DRILLINGen
dc.relation.ispartofseries/ 17 (2014)en
dc.subjectBoreholesen
dc.subjectAltotiberina faulten
dc.subjectNear Fault Observatoryen
dc.titleThe shallow boreholes at The AltotiBerina near fault Observatory (TABOO; northern Apennines of Italy)en
dc.typearticleen
dc.description.statusPublisheden
dc.description.pagenumber31-35en
dc.subject.INGV04. Solid Earth::04.06. Seismology::04.06.01. Earthquake faults: properties and evolutionen
dc.identifier.doi10.5194/sd-17-31-2014en
dc.description.obiettivoSpecifico2T. Sorgente Sismicaen
dc.description.journalTypeJCR Journalen
dc.contributor.authorChiaraluce, Lauroen
dc.contributor.authorCollettini, Cristianoen
dc.contributor.authorCattaneo, Marcoen
dc.contributor.authorMonachesi, Giancarloen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italiaen
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 ONT, Roma, Italia-
crisitem.author.deptUniversità La Sapienza-
crisitem.author.orcid0000-0002-9697-6504-
crisitem.author.orcid0000-0001-6017-8861-
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-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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