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  5. Insights into fluid circulation across the Pernicana Fault (Mt. Etna, Italy) and implications for flank instability
 
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Insights into fluid circulation across the Pernicana Fault (Mt. Etna, Italy) and implications for flank instability

Author(s)
Siniscalchi, A.  
Dipartimento di Geologia e Geofisica, Università degli Studi di Bari, via Orabona, 4-70125, Bari-Italy  
Tripaldi, S.  
Dipartimento di Geologia e Geofisica, Università degli Studi di Bari, via Orabona, 4-70125, Bari-Italy  
Neri, M.  
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia  
Giammanco, S.  
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia  
Piscitelli, S.  
Istituto di Metodologie per l' Analisi Ambientale, CNR, Tito (PZ), Italy  
Balasco, M.  
Istituto di Metodologie per l' Analisi Ambientale, CNR, Tito (PZ), Italy  
Behncke, B.  
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia  
Magri, C.  
Dipartimento di Geologia e Geofisica, Università degli Studi di Bari, via Orabona, 4-70125, Bari-Italy  
Naudet, V.  
Université Bordeaux 1, Geosciences Hydrosciences Material and Constructions, GHYMAC-EA 4134, Talence, F-33405, France  
Rizzo, E.  
Istituto di Metodologie per l' Analisi Ambientale, CNR, Tito (PZ), Italy  
Language
English
Obiettivo Specifico
1.5. TTC - Sorveglianza dell'attività eruttiva dei vulcani
3.2. Tettonica attiva
4.5. Studi sul degassamento naturale e sui gas petroliferi
Status
Published
JCR Journal
JCR Journal
Peer review journal
Yes
Journal
Journal of Volcanology and Geothermal Research  
Issue/vol(year)
/193 (2010)
Publisher
Elsevier B.V.
Pages (printed)
137–142
Date Issued
April 1, 2010
DOI
10.1016/j.jvolgeores.2010.03.013
Alternative Location
http://www.sciencedirect.com/science?_ob=PublicationURL&_tockey=%23TOC%235962%232010%23998069998%231977700%23FLA%23&_cdi=5962&_pubType=J&_auth=y&_acct=C000067082&_version=1&_urlVersion=0&_userid=5381242&md5=fcd41a57ae4a50f631de6ce2810a433a
URI
https://www.earth-prints.org/handle/2122/6035
Subjects
04. Solid Earth::04.02. Exploration geophysics::04.02.99. General or miscellaneous  
04. Solid Earth::04.02. Exploration geophysics::04.02.01. Geochemical exploration  
04. Solid Earth::04.02. Exploration geophysics::04.02.04. Magnetic and electrical methods  
04. Solid Earth::04.02. Exploration geophysics::04.02.05. Downhole, radioactivity, remote sensing, and other methods  
04. Solid Earth::04.02. Exploration geophysics::04.02.07. Instruments and techniques  
04. Solid Earth::04.04. Geology::04.04.99. General or miscellaneous  
04. Solid Earth::04.04. Geology::04.04.06. Rheology, friction, and structure of fault zones  
04. Solid Earth::04.04. Geology::04.04.07. Rock geochemistry  
04. Solid Earth::04.04. Geology::04.04.09. Structural geology  
04. Solid Earth::04.04. Geology::04.04.11. Instruments and techniques  
04. Solid Earth::04.04. Geology::04.04.12. Fluid Geochemistry  
04. Solid Earth::04.07. Tectonophysics::04.07.99. General or miscellaneous  
04. Solid Earth::04.07. Tectonophysics::04.07.07. Tectonics  
04. Solid Earth::04.08. Volcanology::04.08.99. General or miscellaneous  
04. Solid Earth::04.08. Volcanology::04.08.01. Gases  
04. Solid Earth::04.08. Volcanology::04.08.02. Experimental volcanism  
04. Solid Earth::04.08. Volcanology::04.08.04. Thermodynamics  
04. Solid Earth::04.08. Volcanology::04.08.06. Volcano monitoring  
04. Solid Earth::04.08. Volcanology::04.08.07. Instruments and techniques  
04. Solid Earth::04.08. Volcanology::04.08.08. Volcanic risk  
05. General::05.08. Risk::05.08.99. General or miscellaneous  
Subjects

Pernicana Fault

fluid circulation

structural geology

Etna

magnetic

electrical methods

Abstract
We conducted geophysical–geochemical measurements on a ∼2 kmN–S profile cutting across the Pernicana
Fault, one of the most active tectonic features on the NE flank of Mt. Etna. The profile passes from the
unstable E flank of the volcano (to the south) to the stable N flank and significant fluctuations in electrical
resistivity, self-potential, and soil gas emissions (CO2, Rn and Th) are found. The detailed multidisciplinary
analysis reveals a complex interplay between the structural setting, uprising hydrothermal fluids, meteoric
fluids percolating downwards, ground permeability, and surface topography. In particular, the recovered
fluid circulation model highlights that the southern sector is heavily fractured and faulted, allowing the
formation of convective hydrothermal cells. Although the existence of a hydrothermal system in a volcanic
area does not surprise, these results have great implications in terms of flank dynamics at Mt. Etna. Indeed,
the hydrothermal activity, interacting with the Pernicana Fault activity, could enhance the flank instability.
Our approach should be further extended along the full extent of the boundary between the stable and
unstable sectors of Etna for a better evaluation of the geohazard in this active tectonic area.
Sponsors
This work was partly financed by the DPC-INGV FLANK and LAVA
Projects.
References
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