Evidence of active deformation in the adriatic foreland (Southern Italy): integration of onshore and offshore seismotectonic and stratigraphc data along the Molise-Gondola shear zone (Abstract/Poster in atti di convegno)

Type

• Abstract/Poster in atti di convegno (Classe)
• Prodotto della ricerca (Classe)

Label

• Evidence of active deformation in the adriatic foreland (Southern Italy): integration of onshore and offshore seismotectonic and stratigraphc data along the Molise-Gondola shear zone (Abstract/Poster in atti di convegno) (literal)

Anno

• 2006-01-01T00:00:00+01:00 (literal)

Alternative label

• Di Bucci D. (1), Ridente D. (2), Fracassi U. (3), Trincardi F. (2), Valensise G. (3) (2006)
  Evidence of active deformation in the adriatic foreland (Southern Italy): integration of onshore and offshore seismotectonic and stratigraphc data along the Molise-Gondola shear zone
  in 3rd European Geosciences Union General Assembly, Vienna (Austria)
  (literal)

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

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

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

• Geophysical Research Abstracts, Vol. 8, 02146, 2006 SRef-ID: 1607-7962/gra/EGU06-A-02146 (literal)

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

• XY0938 POSTER EGU06-A-02146; TS4.3-1TH1P-0938; (literal)

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

• The active tectonics of the Southern Apennines of Italy (Calabrian Arc excluded) is mainly characterized by SW-NE extension, which accounts for large earthquakes generated by NW-SE striking normal faults. However, the 2002 Molise earthquakes occurred along an E-W striking right-lateral seismogenic structure located to the NE of the Southern Apennines axis, suggesting that the frontal part of the chain and the adjacent foreland are affected by E-W striking, right lateral active faults systems. The 2002 Molise seismic sources are located along the western part of a regional fault system, the Molise-Gondola shear zone (MGsz). On land, this system is mainly represented by the Mattinata Fault, an important structure of the foreland. Off-shore the Gargano Promontory, the Mattinata Fault seems to be aligned with a regional (ca. 150 km in extent) E-W to NW-SE oriented deformation belt (known in the literature as Gondola Line), including a main fault and fold system known as Gondola Fault and Gondola Ridge, respectively. Altogether, both recent seismicity related to E-W dextral strike-slip tectonics along the westernmost part of the MGsz and along the Mattinata Fault itself, and very recent (< 5.5 ka) deformation features along the Gondola Line, suggest that the MGsz as a whole is being actively deformed. To verify this hypothesis, we attempt a comparison between on- and off-shore data supporting recent activity along E-W oriented foreland structures. (literal)

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

• (1) Dipartimento della Protezione Civile - Servizio Sismico Nazionale, Rome, Italy (2) CNR - ISMAR, Sezione di Geologia Marina,Bologna, Italy (3) Istituto Nazionale di Geofisica e Vulcanologia, Rome, Italy (literal)

Titolo

• Evidence of active deformation in the adriatic foreland (Southern Italy): integration of onshore and offshore seismotectonic and stratigraphc data along the Molise-Gondola shear zone (literal)

Prodotto di

• Struttura dei margini continentali, emissione dei fluidi attraverso di essi, e impatto sugli ecosistemi (TA.P02.028.002) (Modulo)
• Institute of environmental geology and geoengineering (IGAG) (Istituto)
• Marine science institute (ISMAR) (Istituto)

Autore CNR

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

Insieme di parole chiave

• Keywords of " Evidence of active deformation in the adriatic foreland (Southern Italy): integration of onshore and offshore seismotectonic and stratigraphc data along the Molise-Gondola shear zone" (Insieme di parole chiave)

Incoming links:

Prodotto

• Institute of environmental geology and geoengineering (IGAG) (Istituto)
• Marine science institute (ISMAR) (Istituto)
• Struttura dei margini continentali, emissione dei fluidi attraverso di essi, e impatto sugli ecosistemi (TA.P02.028.002) (Modulo)

Autore CNR di

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

Insieme di parole chiave di

• Keywords of " Evidence of active deformation in the adriatic foreland (Southern Italy): integration of onshore and offshore seismotectonic and stratigraphc data along the Molise-Gondola shear zone" (Insieme di parole chiave)