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  5. Shear wave splitting changes associated with the 2001 volcanic eruption on Mt. Etna
 
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Shear wave splitting changes associated with the 2001 volcanic eruption on Mt. Etna

Author(s)
Bianco, F.  
Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italia  
Scarfì, L.  
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia  
Del Pezzo, E.  
Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italia  
Patanè, D.  
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia  
Language
English
Status
Published
Peer review journal
Yes
Journal
Geophys. J. Int.  
Issue/vol(year)
/167 (2006)
Pages (printed)
959-967
Date Issued
2006
DOI
10.1111/j.1365-246X.2006.03152.x
URI
https://www.earth-prints.org/handle/2122/2251
Subjects
04. Solid Earth::04.06. Seismology::04.06.07. Tomography and anisotropy  
04. Solid Earth::04.06. Seismology::04.06.09. Waves and wave analysis  
Subjects

cracked media,

seismic anisotropy,

shear wave splitting,...

volcanic activity,

volcanic structure,

wave propagation.

Abstract
The time delays and polarizations of shear wave splitting above small earthquakes show variations
before the 2001 July 17–August 9 2001 flank eruption on Mt Etna, Sicily. Normalized
time delays, measured by singular value decomposition, show a systematic increase starting
several days before the onset of the eruption. On several occasions before the eruption, the
polarization directions of the shear waves at Station MNT, closest to the eruption, show 90◦-
flips where the faster and slower split shear waves exchange polarizations. The last 90◦-flip
being 5 days before the onset of the eruption. The time delays also exhibit a sudden decrease
shortly before the start of the eruption suggesting the possible occurrence of a ‘relaxation’
phenomena, due to crack coalescence. This behaviour has many similarities to that observed
before a number of earthquakes elsewhere.
References
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