Marine paleoseismology from very high resolution seismic imaging: the Gondola Fault Zone (Adriatic Foreland) (Articolo in rivista)

Type

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

Label

• Marine paleoseismology from very high resolution seismic imaging: the Gondola Fault Zone (Adriatic Foreland) (Articolo in rivista) (literal)

Anno

• 2009-01-01T00:00:00+01:00 (literal)

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

• 10.1111/j.1365-3121.2009.00895.x (literal)

Alternative label

• Di Bucci D. 1; Ridente D. 2; Fracassi U. 3; Trincardi F. 4; Valensise G. 3 (2009)
  Marine paleoseismology from very high resolution seismic imaging: the Gondola Fault Zone (Adriatic Foreland)
  in TERRA nova (Print)
  (literal)

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

• Di Bucci D. 1; Ridente D. 2; Fracassi U. 3; Trincardi F. 4; Valensise G. 3 (literal)

Pagina inizio

• 393 (literal)

Pagina fine

• 400 (literal)

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

• 21 (literal)

Rivista

• TERRA nova (Rivista)

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

• IN PRESS (literal)

Note

• ISI Web of Science (WOS) (literal)
• Scopu (literal)

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

• 1. Dipartimento Protez Civile, I-00189 Rome, Italy 2. CNR, Ist Geol Ambientale & Geoingn, I-00185 Rome, Italy 3. Ist Nazl Geofis & Vulcanol, I-00143 Rome, Italy 4. CNR, Ist Sci Marine, I-40129 Bologna, Italy (literal)

Titolo

• Marine paleoseismology from very high resolution seismic imaging: the Gondola Fault Zone (Adriatic Foreland) (literal)

Abstract

• We present a marine palaeoseismology analysis of a dense network of very high resolution seismic profiles along the Gondola Fault Zone (GFZ), a right-lateral, E-W-striking, active fault system in the Adriatic foreland. This case-study aims to show how time and space variations in the activity of a dominantly right-lateral fault system can be assessed using the vertical component of slip. The GFZ has been investigated for a length of 50 km. It includes two parallel subvertical fault sets and two main anticlines. The late Middle Pleistocene to Holocene vertical component of displacement along the fault is bell-shaped, suggesting that in the long-term the fault zone acts as a single, kinematically coherent structure. Slip rates are 0-0.18 mm a

Prodotto di

• Fenomeni di instabilità gravitativa delle aree di piattaforma e di scarpata continentale italiane. (TA.P05.008.002) (Modulo)
• Institute of environmental geology and geoengineering (IGAG) (Istituto)

Autore CNR

• DOMENICO RIDENTE (Unità di personale interno)
• FABIO TRINCARDI (Persona)

Incoming links:

Prodotto

• Institute of environmental geology and geoengineering (IGAG) (Istituto)
• Fenomeni di instabilità gravitativa delle aree di piattaforma e di scarpata continentale italiane. (TA.P05.008.002) (Modulo)

Autore CNR di

• DOMENICO RIDENTE (Unità di personale interno)
• FABIO TRINCARDI (Persona)

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

• TERRA nova (Rivista)