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Akademický článek
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New geological mapping of Stromboli, scale 1:10 000 (southern Italy) as a tool for hazard assessment
A new geological map of Stromboli (southern Italy) at 1:10,000 scale is performed by adopting a modern stratigraphic approach based on lithostratigraphic units (rock types), lithosomes (landforms eruptive centres) and unconformity-bounded units (corr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______4094::3186c89d1e6110786943f32ffe3f5c81
http://hdl.handle.net/11585/387147
http://hdl.handle.net/11585/387147
New stratigraphic data allowed the reconstruction of the activity responsible of the construction of the Monte dei Porri cone. Alternating explosive and effusive activity, which emplaced fall and pyroclastic density current deposits, and lava flows,
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______4094::c71d0e05283aea2e3f83fbcf4f1e93b8
http://hdl.handle.net/11585/387267
http://hdl.handle.net/11585/387267
Vulcano geological history displays several changes of eruption magnitude, eruption styles and composition of magmas through time. Various volcanic edifices and two intersecting multi-stage calderas resulted from such evolution. The collection for ma
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______4094::b3c6edee507b5d2ad79114e9a768fb7d
http://hdl.handle.net/11585/387143
http://hdl.handle.net/11585/387143
Stromboli (southern Italy) is a 924 m-high active composite volcano made up of thick successions of scoriaceous products and lava flows subdivided by erosional discontinuities related to five calderas and seven large-scale lateral collapses (Francala
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______4094::1530ae1b7d84601b551aa20c3e39ad8e
http://hdl.handle.net/11585/387150
http://hdl.handle.net/11585/387150
The Panarea volcanic group is made up of dome-fields that are the subaerial culminations of a largely dissected volcanic complex mostly located below sea level. The correlation of marine isotope stage (MIS) 5 marine terrace deposits and numerous teph
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______4094::946a4998e55f4591755bf9808aa462f9
http://hdl.handle.net/11585/373717
http://hdl.handle.net/11585/373717
Autor:
LUCCHI, FEDERICO, FORNI, FRANCESCA, TRANNE, CLAUDIO ANTONIO, R. Gertisser, J. Keller, G. De Astis
Stratigraphic, structural, volcanological and geochemical data allow a detailed reconstruction of the geological history of the island of Salina (central Aeolian sector). Its subaerial volcanism (~244 ka to 15.6 ka) developed through six successive E
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______4094::9f20c813b7b38798d94593e7b3371818
http://hdl.handle.net/11585/373335
http://hdl.handle.net/11585/373335
A regional framework for stratigraphic correlations in the Aeolian archipelago is provided by widespread tephra layers and Late Quaternary marine terrace deposits combined with the available radiometric ages. Several tephra layers of Campanian and Ae
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______4094::0287ac715d438fa09d0b6b833bce610f
http://hdl.handle.net/11585/373330
http://hdl.handle.net/11585/373330
Autor:
G. De Astis, P. Dellino, L. La Volpe, M. L. Frezzotti, A. Peccerillo, LUCCHI, FEDERICO, TRANNE, CLAUDIO ANTONIO
Vulcano is an active NW–SE-elongated composite volcano located in the central Aeolian archipelago. Based on available radiometric ages and tephrochronology, the exposed volcanism started at c. 127 ka and spread through eight Eruptive Epochs separat
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______4094::d3676f28af5d7bf7662158fdf49cd7fc
http://hdl.handle.net/11585/373338
http://hdl.handle.net/11585/373338