Late quaternary activity along the Scorciabuoi fault (Southern Italy) as inferred from electrical resistivity tomographies (Articolo in rivista)

Type

• Prodotto della ricerca (Classe)
• Articolo in rivista (Classe)

Label

• Late quaternary activity along the Scorciabuoi fault (Southern Italy) as inferred from electrical resistivity tomographies (Articolo in rivista) (literal)

Anno

• 2007-01-01T00:00:00+01:00 (literal)

Alternative label

• Caputo R ,Salviulo L ,Piscitelli S ,Loperte A . (2007)
  Late quaternary activity along the Scorciabuoi fault (Southern Italy) as inferred from electrical resistivity tomographies
  in Annals of geophysics (Testo stamp.)
  (literal)

Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori

• Caputo R ,Salviulo L ,Piscitelli S ,Loperte A . (literal)

Pagina inizio

• 213 (literal)

Pagina fine

• 224 (literal)

Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroVolume

• 50 (literal)

Rivista

• Annals of geophysics (Rivista)

Note

• ISI Web of Science (WOS) (literal)

Titolo

• Late quaternary activity along the Scorciabuoi fault (Southern Italy) as inferred from electrical resistivity tomographies (literal)

Abstract

• The Scorciabuoi Fault is one of the major tectonic structures affecting the Southern Apennines, Italy. Across its central sector, we performed several electrical resistivity tomographics with different electrode spacing (5 and 10 in) 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. (literal)

Prodotto di

• Sviluppo ed integrazione di tecniche di Osservazione della Terra da aereo e da satellite per il monitoraggio della superficie (Terminato) (TA.P06.006.004) (Modulo)
• Istituto di metodologie per l'analisi ambientale (IMAA) (Istituto)

Autore CNR

• SABATINO PISCITELLI (Unità di personale interno)
• ANTONIO LOPERTE (Unità di personale esterno)

Insieme di parole chiave

• Keywords of "Late quaternary activity along the Scorciabuoi fault (Southern Italy) as inferred from electrical resistivity tomographies" (Insieme di parole chiave)

Incoming links:

Autore CNR di

• SABATINO PISCITELLI (Unità di personale interno)
• ANTONIO LOPERTE (Unità di personale esterno)

Prodotto

• Istituto di metodologie per l'analisi ambientale (IMAA) (Istituto)
• Sviluppo ed integrazione di tecniche di Osservazione della Terra da aereo e da satellite per il monitoraggio della superficie (Terminato) (TA.P06.006.004) (Modulo)

Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#rivistaDi

• Annals of geophysics (Rivista)

Insieme di parole chiave di

• Keywords of "Late quaternary activity along the Scorciabuoi fault (Southern Italy) as inferred from electrical resistivity tomographies" (Insieme di parole chiave)