The Lipari volcanic complex, situated in the central Aeolian sector, was constructed between c. 267 ka and medieval ages by various lava flows, scoriaceous deposits, lava domes (coulees) and pyroclastic products related to hydromagmatic and strombolian activities. The eruptive history of Lipari is described by nine Epochs of activity interrupted by dormant periods, volcano-tectonic phases and episodes of terrace formation during the Last Interglacial.
Forni, F., Lucchi, F., Peccerillo, A., Tranne, C., Rossi, P., Frezzotti, M. (2013). Stratigraphy and geological evolution of the Lipari volcanic complex (central Aeolian archipelago). In The Aeolian Islands volcanoes (pp. 213-279). The Geological Society, London Memoirs [10.1144/M37.10].
Stratigraphy and geological evolution of the Lipari volcanic complex (central Aeolian archipelago)
FREZZOTTI, MARIA LUCE
2013
Abstract
The Lipari volcanic complex, situated in the central Aeolian sector, was constructed between c. 267 ka and medieval ages by various lava flows, scoriaceous deposits, lava domes (coulees) and pyroclastic products related to hydromagmatic and strombolian activities. The eruptive history of Lipari is described by nine Epochs of activity interrupted by dormant periods, volcano-tectonic phases and episodes of terrace formation during the Last Interglacial.
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