http://www.cnr.it/ontology/cnr/individuo/prodotto/ID7006
Stratigraphic and structural setting of the Ischia volcanic complex (Naples Bay, southern Italy) revealed by submarine seismic reflection data (Articolo in rivista)
- Type
- Label
- Stratigraphic and structural setting of the Ischia volcanic complex (Naples Bay, southern Italy) revealed by submarine seismic reflection data (Articolo in rivista) (literal)
- Anno
- 2012-01-01T00:00:00+01:00 (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#doi
- 10.1007/s12210-012-0204-2 (literal)
- Alternative label
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- Gemma Aiello; Ennio Marsella; Salvatore Passaro (literal)
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- Articolo ISI su rivista internazionale con referee internazionale (literal)
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- Rivista
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- lavoro sottomesso per la stampa in corso di referaggio (literal)
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- articolo ISI su rivista internazionale con referee (literal)
- Note
- ISI Web of Science (WOS) (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
- CNR-IAMC Sede di Napoli (literal)
- Titolo
- Stratigraphic and structural setting of the Ischia volcanic complex (Naples Bay, southern Italy) revealed by submarine seismic reflection data (literal)
- Abstract
- High resolution seismic reflection profiles (Sparker Multitip) offshore southern Ischia island (Naples Bay) are here presented, together with a geological interpretation of their volcanic, structural and sedimentary features. In this frame, new seismo-stratigraphic evidences on buried volcanic structures and overlying Quaternary deposits of the south-eastern offshore of Ischia island are discussed to highlight their implications on the marine geophysics and volcanology. The Ischia Bank is a large and flat relic volcanic edifice with steep slopes, merging on the continental shelf. The age of this monogenic volcano is unknown, lacking a direct datation of its basement. It represents the eruptive centre of the pyroclastic fall cropping out onshore in the eastern sector of the island, ranging in age from 8 to 6 ky B.P.. In the eastern Ischia offshore relic volcanic edifices, mostly formed by hialoclastites, have been investigated through high resolution seismics. They represent remnants of hydro-magmatic volcanic vents and suggest a subaqueous emplacement. Regional seismic sections running in the south-eastern Ischia offshore, across buried volcanic structures, are finally presented and discussed. (literal)
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