Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/4831
AuthorsDe Vita, S.* 
Sansivero, F.* 
Orsi, G.* 
Marotta, E.* 
Piochi, M.* 
TitleVolcanological and structural evolution of the Ischia resurgent caldera (Italy) over the past 10 ka.
Issue Date2008
URIhttp://hdl.handle.net/2122/4831
KeywordsVolcanological
Ischia resurgent
Subject Classification04. Solid Earth::04.08. Volcanology::04.08.05. Volcanic rocks 
04. Solid Earth::04.08. Volcanology::04.08.08. Volcanic risk 
05. General::05.02. Data dissemination::05.02.03. Volcanic eruptions 
AbstractVolcanic activity on the island of Ischia included both effusive and explosive eruptions, mainly occurred in the eastern sector of the island. Vent location, eruption dynamics, transport mechanisms and depositional processes, have been reconstructed for each recognized unit. In the past 10 ka, periods of quiescence alternated with periods of very intense volcanism, which was mainly concentrated at about 5.5 and over the past 2.9 ka. Volcanism was not continuous and strongly influenced by the mechanism of a resurgence phenomenon, which affects the island since about 33 ka. Therefore, it has been hypothesized that magma intrusion and uplift events occurred intermittently. In the past 5.5 ka, volcanic activity has been invariably accompanied by the emplacement of slope instability-related deposits testifying that also slope instability was induced by reactivation of vertical movements, likely related to resurgence.
Appears in Collections:Papers Published / Papers in press

Files in This Item:
File Description SizeFormat 
DeVSan-08.pdf14.56 MBAdobe PDFView/Open
Show full item record

Page view(s)

193
Last Week
0
Last month
0
checked on Aug 23, 2017

Download(s)

58
checked on Aug 23, 2017

Google ScholarTM

Check