The western undersea section of the Ischia volcanic complex (Italy, Tyrrhenian sea) inferred from marine geophysical data (Articolo in rivista)

Type

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

Label

• The western undersea section of the Ischia volcanic complex (Italy, Tyrrhenian sea) inferred from marine geophysical data (Articolo in rivista) (literal)

Anno

• 2002-01-01T00:00:00+01:00 (literal)

Alternative label

• Bruno P. P., de Alteriis G., Florio G., (2002)
  The western undersea section of the Ischia volcanic complex (Italy, Tyrrhenian sea) inferred from marine geophysical data
  in Geophysical research letters
  (literal)

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

• Bruno P. P., de Alteriis G., Florio G., (literal)

Pagina inizio

• 1029 (literal)

Pagina fine

• 1034 (literal)

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

• 29/9 (literal)

Rivista

• Geophysical research letters (Rivista)

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

• Geophysical and geological exploration of the undersea sectors off the Ischia island active volcano (literal)

Note

• ISI Web of Science (WOS) (literal)

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

• Osservatorio Vesuviano, INGV, Napoli IAMC, Geomare sud, CNR, Napoli Dipartimento Scienze della Terra, Università Federico II, Napoli (literal)

Titolo

• The western undersea section of the Ischia volcanic complex (Italy, Tyrrhenian sea) inferred from marine geophysical data (literal)

Abstract

• Ischia Island represents only the remnant of a larger volcanic complex. To prove this hypothe-sis about 600 km of new marine and geophysical data were utilized. Results reveal that the western offshore of the island is mainly made by previously unreported E-W and NE-SW ridges that include several volcanic edifices. Interpretation of sea-borne magnetic data evi-dences a, good correlation between bathymetry and magnetic anomalies, indicating the presence of a larger volcanic system than what previously known, with evidences of deeper in-trusions of cooled magma. The deeper intrusions show NE-SW trends. Subvertical NE faults, visible on seismic and CHIRP data, delimit the volcanic ridges to the NW and upthrow the vol-canic basement towards the Island. Geophysical data indicate that the age of faulting is extremely recent and seem not triggered by volcanism. Tectonically controlled uplift phenomena outside the Ischia caldera raise doubts on the current interpretation of Mt. Epomeo as a resurgent dome. (literal)

Prodotto di

• Institute for coastal marine environment (IAMC) (Istituto)

Insieme di parole chiave

• Parole chiave di "The western undersea section of the Ischia volcanic complex (Italy, Tyrrhenian sea) inferred from marine geophysical data" (Insieme di parole chiave)

Incoming links:

Prodotto

• Institute for coastal marine environment (IAMC) (Istituto)

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

• Geophysical research letters (Rivista)

Insieme di parole chiave di

• Parole chiave di "The western undersea section of the Ischia volcanic complex (Italy, Tyrrhenian sea) inferred from marine geophysical data" (Insieme di parole chiave)