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Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/361

Authors: Barberi, G.*
Cocina, O.*
Maiolino, V.*
Musumeci, C.*
Privitera, E.*
Title: Insight into Mt. Etna (Italy) kinematics during the 2002–2003 eruption as inferred from seismic stress and strain tensors
Title of journal: Geophysical Research Letters
Series/Report no.: 21/31(2004)
Publisher: AGU
Issue Date: 13-Nov-2004
DOI: 10.1029/2004GL020918
Keywords: Seismology: Seismicity and seismotectonics
Seismology: Volcano seismology
Volcanology: Eruption mechanisms
Volcanology: Magma migration
Abstract: Seismic activity linked to the 2002–03 Mt. Etna eruption was investigated by analyzing the Md > 2.3 earthquakes. The results of 3D relocation were used to compute fault plane solutions and a selected dataset was inverted to determine stress and strain tensors. The analysis revealed a complex kinematic response of the eastern flank dominated by fast stress propagation and reorientation. We hypothesize that a vertical dike intruded the southern flank, generating an extensional regime that triggered a radial intrusion in the northeast sector of the volcano. The combined effects gave rise to a rotation of the stress tensor that controlled the activation of the Pernicana fault system. The volcanic and tectonic interactions produced a second reorientation of the stress tensor, causing a structural response in the southeast lower flank. The overall result of the deformation processes observed during the eruption was an E-W extension on the eastern flank of the volcano.
Appears in Collections:04.06.08. Volcano seismology
Papers Published / Papers in press

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