Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/6969
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dc.contributor.authorallPierdominici, S.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.authorallMariucci, M. T.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.authorallMontone, P.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.date.accessioned2011-03-25T06:54:29Zen
dc.date.available2011-03-25T06:54:29Zen
dc.date.issued2011-01-19en
dc.identifier.urihttp://hdl.handle.net/2122/6969en
dc.description.abstractIdentification of an active fault and the local versus regional present-day stress field in the Irpinia region (southern Apennines) have been performed along a 5900m deep well (San Gregorio Magno 1) by a detailed breakout and geophysical log analysis. The selected area is characterized by diffuse low magnitude seismicity, although in historical times moderate to large earthquakes have repeatedly struck it. On 23rd November 1980 a strong earthquake (M=6.9) nucleated on a 38km-long normal fault, named Irpinia fault, producing the first unequivocal historical surface faulting ever documented in Italy. The analysis of stress-induced wellbore breakouts shows a direction of minimum horizontal stress N18°±24°, fairly consistent with the regional stress trend (N44°±20°). The small discrepancy between our result and the regional stress orientation might be related to the influence of local stress sources such as variations of the Irpinia fault plane orientation and the presence of differently oriented active shear zones. This paper shows for the first time a detailed analysis on the present-day stress along a well to identify the Irpinia fault at depth and constrain its geometry.en
dc.language.isoEnglishen
dc.relation.ispartofJournal of Geodynamicsen
dc.relation.ispartofseries3-4/52 (2011)en
dc.subjectBorehole breakouten
dc.subjectGeophysical logen
dc.subjectPresent-day stress fielden
dc.subjectSeismogenic faulten
dc.subjectSouthern Apenninesen
dc.subjectItalyen
dc.titleA study to constrain the geometry of an active fault in southern Italy through borehole breakouts and downhole logsen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.subject.INGV04. Solid Earth::04.07. Tectonophysics::04.07.05. Stressen
dc.identifier.doi10.1016/j.jog.2011.02.006en
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dc.description.obiettivoSpecifico3.2. Tettonica attivaen
dc.description.journalTypeJCR Journalen
dc.description.fulltextreserveden
dc.contributor.authorPierdominici, S.en
dc.contributor.authorMariucci, M. T.en
dc.contributor.authorMontone, P.en
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
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item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
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crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia-
crisitem.author.orcid0000-0002-5368-4536-
crisitem.author.orcid0000-0001-6029-1514-
crisitem.author.orcid0000-0002-9297-1730-
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-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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