Please use this identifier to cite or link to this item: https://www.um.edu.mt/library/oar/handle/123456789/45634
Title: Deep crustal faults and the origin and long-term flank stability of Mt. Etna : first results from the CIRCEE cruise (Oct. 2013)
Authors: Gutscher, Marc-Andre
Dominguez, Stephane
Lepinay, Bernard Mercier de
Pinheiro, Luis
Babonneau, Nathalie
Cattaneo, Antonio
LeFaou, Yann
Barreca, Giovanni
Micallef, Aaron
Rovere, Marzia
Keywords: Etna, Mount (Italy)
Geology, Structural -- Italy -- Sicily
Geodynamics -- Italy -- Sicily
Geophysics -- Italy -- Sicily
Geomorphology -- Italy -- Sicily
Faults (Geology) -- Italy -- Sicily
Issue Date: 2014
Publisher: Copernicus GmbH
Citation: Gutscher, M. A., Dominguez, S., Mercier de Lepinay, B., Pinheiro, L., Babonneau, N., Cattaneo, A., ... & Rovere, M. (2014). Deep crustal faults and the origin and long-term flank stability of Mt. Etna: First results from the CIRCEE cruise (Oct. 2013). Geophysical Research Abstracts, 16
Abstract: The relation between deep crustal faults and the origin of Mount Etna, the largest and most active volcano in Europe has long been suspected due to its unusual geodynamic location. Results from a new marine geophysical survey offshore Eastern Sicily reveal the detailed geometry (location, length, dip and orientation) of a two-branched 200-km long, lithospheric scale fault system, long sought for as being the cause of Mount Etna. Using high-resolution bathymetry and seismic profiling, we image a 60-km long, previously unidentified, NW trending fault with evidence of recent displacement at the seafloor, offsetting Holocene sediments. This newly identified fault connects NE of Catania, to a known 40-km long, offshore-onshore fault system dissecting the southeastern flank of Mount Etna, generally interpreted as purely gravitational collapse structures.
URI: https://www.um.edu.mt/library/oar/handle/123456789/45634
ISSN: 16077962
Appears in Collections:Scholarly Works - FacSciGeo

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