http://www.cnr.it/ontology/cnr/individuo/prodotto/ID49040
Sedimentologic and volcanologic investigation of the deep Tyrrhenian Sea: preliminary results of cruise VST02. (Articolo in rivista)
- Type
- Label
- Sedimentologic and volcanologic investigation of the deep Tyrrhenian Sea: preliminary results of cruise VST02. (Articolo in rivista) (literal)
- Anno
- 2006-01-01T00:00:00+01:00 (literal)
- Alternative label
Gamberi F. (1), Marani M. (1), Landuzzi V. (1), Magagnoli A. (1), Penitenti D. (1), Rosi M. (2), Bertagnini A. (2), Di Roberto A. (2) (2006)
Sedimentologic and volcanologic investigation of the deep Tyrrhenian Sea: preliminary results of cruise VST02.
in Annals of geophysics (Testo stamp.)
(literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
- Gamberi F. (1), Marani M. (1), Landuzzi V. (1), Magagnoli A. (1), Penitenti D. (1), Rosi M. (2), Bertagnini A. (2), Di Roberto A. (2) (literal)
- Pagina inizio
- Pagina fine
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#altreInformazioni
- http://www.earth-prints.org/bitstream/2122/1071/6/16+Gamberi.pdf. (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroVolume
- Rivista
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#note
- Issue 2/3, April/June (literal)
- Note
- ISI Web of Science (WOS) (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
- (1) Istituto di Scienze Marine (ISMAR), CNR, Sezione di Geologia Marina, Bologna, Italy
(2) Dipartimento di Scienze della Terra, Università degli Studi di Pisa, Italy
(3) Istituto Nazionale di Geofisica e Vulcanologia, Sede di Pisa, Italy (literal)
- Titolo
- Sedimentologic and volcanologic investigation of the deep Tyrrhenian Sea: preliminary results of cruise VST02. (literal)
- Abstract
- The VST02 cruise carried out in the summer of 2002 focused on sedimentologic and volcanologic research over
selected areas of the deep portion of the Tyrrhenian Sea. Chirp lines and seafloor samples were collected from
the Calabrian slope surrounding Stromboli Island, in the Marsili deep-sea fan, in the Vavilov Basin and in the
Vavilov seamount. Submarine volcanic activity, both explosive and effusive, is occurring in the Stromboli edi-
fice. Explosive submarine volcanism also affects the shallowest areas of the Vavilov seamount. Submarine car-
bonate lithification has been observed on the sediment-starved flanks of the Vavilov seamount. Acoustic trans-
parent layers make up the recentmost infill of the Gortani Basin, the easternmost portion of the Vavilov Basin.
Channels comprised of a variety of architectural elements and depositional lobes are the main elements of the
Marsili deep-sea fan where, apparently, sedimentation occurs mainly through debris flow processes. (literal)
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