Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/3522
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dc.contributor.authorallCaputo, R.; Dipartimento di Scienze della Terra, Università degli Studi di Ferrara, Italyen
dc.contributor.authorallSalviulo, L.; Dipartimento di Strutture, Geotecnica, Geologia Applicata all’Ingegneria (DiSGG)en
dc.contributor.authorallPiscitelli, S.; Istituto di Metodologie per l'Analisi Ambientale (IMAA)-CNR, Tito Scalo (PZ), Italyen
dc.contributor.authorallLoperte, A.; Istituto di Metodologie per l'Analisi Ambientale (IMAA)-CNR, Tito Scalo (PZ), Italyen
dc.date.accessioned2007-12-31T09:32:55Zen
dc.date.available2007-12-31T09:32:55Zen
dc.date.issued2007-04en
dc.identifier.urihttp://hdl.handle.net/2122/3522en
dc.description.abstractThe Scorciabuoi Fault is one of the major tectonic structures affecting the Southern Apennines, Italy. Across its central sector, we performed several electrical resistivity tomographies with different electrode spacing (5 and 10 m) and using a multielectrode system with 32 electrodes. All tomographies were acquired with two different arrays, the dipole-dipole and the Wenner-Schlumberger. We also tested the different sensitivity of the two arrays with respect to the specific geological conditions and research goals. Detailed geological mapping and two boreholes were used to calibrate the electrical stratigraphy. In all but one tomography (purposely performed off the fault trace), we could recognise an abrupt subvertical lateral variation of the main sedimentary bodies showing the displacement and sharp thickening of the two youngest alluvial bodies in the hanging-wall block. These features are interpreted as evidence of synsedimentary activity of the Scorciabuoi Fault during Late Pleistocene and possibly as recently as Holocene and allow accurate location of the fault trace within the Sauro alluvial plain.en
dc.language.isoEnglishen
dc.relation.ispartofseries2/50 (2007)en
dc.subjectactive tectonicsen
dc.subjectApenninesen
dc.subjectgeoelectrical surveyen
dc.subjectHoloceneen
dc.subjectVal d’Agrien
dc.titleLate Quaternary activity along the Scorciabuoi Fault (Southern Italy) as inferred from electrical resistivity tomographiesen
dc.typearticleen
dc.type.QualityControlPeer-revieweden
dc.subject.INGV04. Solid Earth::04.06. Seismology::04.06.07. Tomography and anisotropyen
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dc.description.journalTypeJCR Journalen
dc.description.fulltextopenen
dc.contributor.authorCaputo, R.en
dc.contributor.authorSalviulo, L.en
dc.contributor.authorPiscitelli, S.en
dc.contributor.authorLoperte, A.en
dc.contributor.departmentDipartimento di Scienze della Terra, Università degli Studi di Ferrara, Italyen
dc.contributor.departmentDipartimento di Strutture, Geotecnica, Geologia Applicata all’Ingegneria (DiSGG)en
dc.contributor.departmentIstituto di Metodologie per l'Analisi Ambientale (IMAA)-CNR, Tito Scalo (PZ), Italyen
dc.contributor.departmentIstituto di Metodologie per l'Analisi Ambientale (IMAA)-CNR, Tito Scalo (PZ), Italyen
item.cerifentitytypePublications-
item.languageiso639-1en-
item.fulltextWith Fulltext-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.grantfulltextopen-
item.openairetypearticle-
crisitem.classification.parent04. Solid Earth-
crisitem.author.deptUniversità degli Studi di Ferrara, Dipartimento di Scienze della Terra. Via Saragat, 1 – 44100 Ferrara, Italy-
crisitem.author.deptDipartimento di Strutture, Geotecnica, Geologia Applicata all’Ingegneria (DiSGG)-
crisitem.author.deptIMAA CNR Potenza-
crisitem.author.deptIstituto di Metodologie per l'Analisi Ambientale (IMAA)-CNR, Tito Scalo (PZ), Italy-
crisitem.author.orcid0000-0002-8884-8991-
Appears in Collections:Annals of Geophysics
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