Tectonics and crustal structure of the Campania continental margin: relationships with volcanism (Articolo in rivista)

Type

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

Label

• Tectonics and crustal structure of the Campania continental margin: relationships with volcanism (Articolo in rivista) (literal)

Anno

• 2003-01-01T00:00:00+01:00 (literal)

Alternative label

• Milia A. , Torrente M.;., Russo M., Zuppetta A (2003)
  Tectonics and crustal structure of the Campania continental margin: relationships with volcanism
  in Mineralogy and petrology
  (literal)

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

• Milia A. , Torrente M.;., Russo M., Zuppetta A (literal)

Pagina inizio

• 33 (literal)

Pagina fine

• 47 (literal)

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

• 79 (literal)

Rivista

• Mineralogy and petrology (Rivista)

Note

• ISI Web of Science (WOS) (literal)

Titolo

• Tectonics and crustal structure of the Campania continental margin: relationships with volcanism (literal)

Abstract

• The crustal structure of the Campania continental margin is synthesised from outcrop, seismic reflection and gravimetric data. Outcrop and subsurface geologic data reveal the presence of NE-SW faults, E-W faults and NW-SE faults. An older extensional event occured along NW-SE faults and was followed by the main extensional event linked to the activity of NE-SW normal faults. The latter were active between 700 and 400 ka producing half-grabens filled by more than 5 km of Quaternary deposits. The stratigraphic signature of these tectonic events corresponds to a Lower Pleistocene marine unconformity-bounded unit overlain by a Middle Pleistocene transgressive-regressive cycle. A crustal section of the Campania margin displays an asymmetric linked fault system characterized by a 10-12 km-deep main detachement level, listric normal faults and rollover anticlines. Structural and stratigraphic data document that the inception of volcanic activity at Vesuvius occured 400 ka, just after the main extensional event, and the volcano position is at the margin of a rollover anticline. (literal)

Prodotto di

• Assetto geologico di siti mediterranei ed oceanici e rischi connessi nelle aree costiere (TA.P01.011.001) (Modulo)
• Institute for coastal marine environment (IAMC) (Istituto)

Autore CNR

• ALFONSA MILIA (Unità di personale interno)

Insieme di parole chiave

• Parole chiave di "Tectonics and crustal structure of the Campania continental margin: relationships with volcanism" (Insieme di parole chiave)

Incoming links:

Prodotto

• Institute for coastal marine environment (IAMC) (Istituto)
• Assetto geologico di siti mediterranei ed oceanici e rischi connessi nelle aree costiere (TA.P01.011.001) (Modulo)

Autore CNR di

• ALFONSA MILIA (Unità di personale interno)

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

• Mineralogy and petrology (Rivista)

Insieme di parole chiave di

• Parole chiave di "Tectonics and crustal structure of the Campania continental margin: relationships with volcanism" (Insieme di parole chiave)