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|Authors: ||Bonforte, A.*|
|Title: ||Multidisciplinary geophysical study of the NE sector of the unstable flank of Etna volcano|
|Issue Date: ||12-Apr-2015|
|Keywords: ||geodesy, seismology, magnetotelluric, flank instability|
|Abstract: ||On volcanic areas, usually characterized by complex structural environments, a lot of independent geophysical
studies are usually performed. The non-uniqueness of the geophysical inverse models, the different level of reso-
lution and sensitivity of the results spurred us to integrate independent geophysical datasets and results collected
on Mt. Etna volcano, in order to obtain more accurate and reliable model interpretation.
Mt. Etna volcano is located along the eastern coast of Sicily and it is characterized by a complex structural set-
ting. In this region, the general N-S compressive regime related to the Africa – Europe collision interacts with the
WNW-ESE extensional regime associated to the Malta Escarpment dynamics, observable along the eastern coast
At Mt Etna, a great number of studies concerns the existence of instability phenomena; a general eastward mo-
tion of the eastern ﬂank of the volcano has been measured with always increasing detail and its relationship with
the eruptive and magmatic activity is being investigated. The unstable ﬂank appears bounded to the north by the
E–W-trending Provenzana - Pernicana Fault System and to the SW by the NS Ragalna Fault system. Eastwards,
this area is divided by several NW–SE trending faults. Recent studies consider this area as divided into several
blocks characterized by different shape and kinematics. Ground deformation studies (GPS and InSAR) deﬁne the
NE portion of the unstable ﬂank as the most mobile one.
In the frame of the MEDiterranean Supersites Volcanoes (MED-SUV) project, ground deformation data (GPS and
INSAR), 3D seismicity, seismic tomography and two resistivity model proﬁles, have been analyzed together, in
order to put some constraints on the deep structure of the NE sector of the unstable ﬂank.
Seismic data come from the permanent network run by the Istituto Nazionale di Geoﬁsica e Vulcanologia (INGV)
- Sezione di Catania, Osservatorio Etneo.
Ground deformation data comes from InSAR Permanent Scatterers analyses of different spaceborn sensors.
The resistivity models come from a MT survey carried out on the eastern ﬂank of the volcano and consisting of
thirty broad-band soundings along N-S and NW-SE oriented proﬁles.
We found that the NE sector of the sliding volume, modeled by ground deformation data inversions and character-
ized by the highest displacement velocity, is characterized low resistivity values and it is bounded by two seismic
clusters. The northern one is clearly related to the Pernicana fault and it’s not deeper than 3 km b.s.l. while the
second one is located southwards, beneath the northern wall of the Valle del Bove, not related to any evident struc-
ture at the surface. An evident layer with very reduced seismicity lies at 3 km of depth and well corresponds to the
simpliﬁed analytic models of a sliding planar surface resulting from GPS data inversions.|
|Appears in Collections:||04.03.99. General or miscellaneous|
04.02.04. Magnetic and electrical methods
04.06.99. General or miscellaneous
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