http://www.cnr.it/ontology/cnr/individuo/prodotto/ID28592
Occurrence of Somma-Vesuvio fine ashes in the tephrostratigraphic record of Panarea, Aeolian Islands (Articolo in rivista)
- Type
- Label
- Occurrence of Somma-Vesuvio fine ashes in the tephrostratigraphic record of Panarea, Aeolian Islands (Articolo in rivista) (literal)
- Anno
- 2008-01-01T00:00:00+01:00 (literal)
- Alternative label
De Rita D., Dolfi D., Cimarelli C. (2008)
Occurrence of Somma-Vesuvio fine ashes in the tephrostratigraphic record of Panarea, Aeolian Islands
in Journal of volcanology and geothermal research
(literal)
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- De Rita D., Dolfi D., Cimarelli C. (literal)
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- Pagina fine
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- Rivista
- Note
- ISI Web of Science (WOS) (literal)
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- Dipartimento di Scienze Geologiche, Università degli Studi Roma Tre (literal)
- Titolo
- Occurrence of Somma-Vesuvio fine ashes in the tephrostratigraphic record of Panarea, Aeolian Islands (literal)
- Abstract
- Southern Italy) have been analyzed and related to their original volcanic sources. One of these tephra layers is
particularly important as it can be correlated by its chemical and morphoscopic characteristics to the
explosive activity of Somma-Vesuvio. Correlation with the Pomici di Base eruption, that is considered one of
the largest explosive events causing the demolition of the Somma stratovolcano, seems the most probable.
The occurrence on Panarea island of fine ashes related to this eruption is of great importance for several
reasons: 1) it allows to better constrain the time stratigraphy of the Panarea volcano; 2) it provides a useful
tool for tephrochronological studies in southern Italy and finally 3) it allows to improve our knowledge on
the distribution of the products of the Pomici di Base eruption giving new insights on the dispersion
trajectories of fine ashes from plinian plumes. Other exotic tephra layers interbedded in the Panarea
pyroclastic successions have also been found. Chemical and sedimentological characteristics of these layers
allow their correlation with local vents from the Aeolian Islands thus constraining the late explosive activity
of Panarea dome (literal)
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