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High precision tilt observation at Mt. Etna Volcano, Italy

Wybrane pełne teksty z tego czasopisma
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Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
In 2007-2008, we installed on Mt. Etna two deep tilt stations using high resolution, self-leveling instruments. These installations are a result of accurate instrument tests, site selection, drilling and sensor positioning that has allowed detecting variations related to the principal diurnal and semidiurnal tides for first time on Mt. Etna using tilt data. We analyzed the tidal effects recorded on tilt signals and we removed tidal effects from signals, thereby allowing to detect changes of about 20 nrad with a considerable improvement in respect to the previous installation. Tilt changes have accompanied the Mt. Etna main eruptive phases and are generally related to the rapid rise of magma and formation of dikes and eruptive fissures. However, tilt changes may characterize lava fountains, earthquakes, and inflation-deflation phases. The 2008-2009 eruption represents an example of the potential of the tiltmeters we used, which provides new perspectives for highly precise monitoring of ground deformation on volcanoes.
Czasopismo
Rocznik
Strony
618--632
Opis fizyczny
Bibliogr. 39 poz.
Twórcy
autor
autor
autor
autor
autor
autor
  • Istituto Nazionale di Geofisica e Vulcanologia, Sezione di Catania, Catania, Italy, gambino@ct.ingv.it
Bibliografia
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  • Aloisi, M., A. Bonaccorso, S. Gambino, M. Mattia, and G. Puglisi (2003), Etna 2002 eruption imaged from continuous tilt and GPS data, Geophys. Res. Lett. 30, 23, 2214, DOI: 10.1029/2003GL018896.
  • Aloisi, M., A. Bonaccorso, and S. Gambino (2006), Imaging composite dike propagation (Etna, 2002 case), J. Geophys. Res. 111, B06404, DOI: 10.1029/2005JB003908.
  • Aloisi, M., A. Bonaccorso, F. Cannavò, S. Gambino, M. Mattia, G. Puglisi, and E. Boschi (2009), A new dyke intrusion style for the Mount Etna May 2008 eruption modelled through continuous tilt and GPS data, Terra Nova 21, 4, 316-321, DOI: 10.1111/j.1365-3121.2009.00889.x.
  • Alparone, S., and S. Gambino (2003), High precision locations of multiplets on southeastern flank of Mt. Etna (Italy): reconstruction of fault plane geometry, Phys. Earth Plan. Int. 135, 4, 281-289, DOI: 10.1016/S0031-9201(03)00048-7.
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  • Bonaccorso, A., and S. Gambino (1997), Impulsive tilt variations on Mount Etna Volcano (1990-1993), Tectonophysics 270, 1-2, 115-125, DOI: 10.1016/S0040-1951(96)00172-2.
  • Bonaccorso, A., G. Falzone, and S. Gambino (1999), An investigation into shallow borehole tiltmeters, Geophys. Res. Lett. 26, 11, 1637-1640, DOI: 10.1029/1999GL900310.
  • Bonaccorso, A., O. Campisi, G. Falzone, and S. Gambino (2004), Continuous tilt monitoring: lesson from 20 years experience at Mt. Etna. In: A. Bonaccorso, S. Calvari, M. Coltelli, C. Del Negro, and S. Falsaperla (eds.), Mt. Etna: Volcano Laboratory, American Geophysical Union, Washington D.C., 307-320, DOI: 10.1029/143GM19.
  • Bonaccorso, A., S. Gambino, F. Guglielmino, M. Mattia, G. Puglisi, and E. Boschi (2008), Stromboli 2007 eruption: Deflation modeling to infer shallowintermediate plumbing system, Geophys. Res. Lett. 35, L06311, DOI: 10.1029/2007GL032921.
  • Bonforte, A., S. Gambino, F. Guglielmino, F. Obrizzo, M. Palano, and G. Puglisi (2007), Ground deformation modeling of flank dynamics prior to the 2002 eruption of Mt. Etna, Bull. Volcanol. 69, 7, 757-768, DOI: 10.1007/s00445-006-0106-1.
  • Bonforte, A., S. Gambino, and M. Neri (2009), Intrusion of eccentric dikes: The case of the 2001 eruption and its role in the dynamics of Mt. Etna volcano, Tectonophysics 471, 1-2, 78-86, DOI: 10.1016/j.tecto.2008.09.028.
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Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BSL7-0049-0022
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