Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/2206
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dc.contributor.authorallBonaccorso, A.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Catania, Catania, Italiaen
dc.date.accessioned2007-07-03T07:17:39Zen
dc.date.available2007-07-03T07:17:39Zen
dc.date.issued2006en
dc.identifier.urihttp://hdl.handle.net/2122/2206en
dc.description.abstractWe investigated the relationships between modelled strain produced by explosive activity through a volcanic conduit, observed paroxystic episodes on Mt. Etna, and high-precision continuous tilt signals recorded during such events from the tilt monitoring network. The tilt changes detected during two different explosive episodes were compared with those calculated from analytical models of ground deformation in order to constrain source properties. The July 22, 1998 subplinian explosion from Voragine crater produced small tilt changes (order of 0.5–1.5 μrad) recorded over the entire volcano edifice, implying a small storage at nearly 2.5 km below sea level. The 1998–2000 period was characterized by tens of spectacular lava fountains from the South-East crater. Very small tilt change (∼ 0.1 μrad) was recorded by a single station on the high north-eastern flank of Mt. Etna and indicated the action of a limited and shallow conduit with 1.5–1.9 km depth. These results provide a contribution to better infer the shallow plumbing system beneath Mt. Etna.en
dc.format.extent1124063 bytesen
dc.format.mimetypeapplication/pdfen
dc.language.isoEnglishen
dc.publisher.nameElsevieren
dc.relation.ispartofJournal of Volcanology and Geothermal Researchen
dc.relation.ispartofseries/158 (2006)en
dc.subjectexplosive activityen
dc.subjecttilt dataen
dc.subjectvolcano source modelingen
dc.subjectMt. Etnaen
dc.titleExplosive activity at mt. etna summit craters and source modeling by using high precision continuous tilten
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber221–234en
dc.identifier.URLwww.siencedirect.comen
dc.subject.INGV04. Solid Earth::04.08. Volcanology::04.08.06. Volcano monitoringen
dc.subject.INGV05. General::05.02. Data dissemination::05.02.03. Volcanic eruptionsen
dc.identifier.doi10.1016/j.jvolgeores.2006.05.007en
dc.relation.referencesAllard, P., Burton, M., Murè, F., 2005. Spectroscopic evidence for lava fountain driven by previously accumulated magmatic gas. Nature 433, 407–409. Aloisi, M., D'Agostino, M., Dean, K.G., Mostaccio, A., Neri, G., 2002. Satellite analysis and PUFF simulation of the eruptive cloud generated by the Mount Etna paroxysmof 22 July 1998. J. Geophys. Res. 107 (B12), 2373. doi:10.1029/2001JB000630. Andronico, D., Del Carlo, P., Coltelli, M., 1999. The 22 July 199.8 fire fountain episode at Voragine Crater (Mt. Etna, Italy). VMSG — Oral presentation at Volcanic and Magmatic Studies Group, Annual Meeting, Birmingham, January 5–6, 1999. Alparone, S., Andronico, D., Lodato, L., Sgroi, T., 2003. Relationship between tremor and volcanic activity during the Southeast Crater eruption on Mount Etna in early 2000. J. Geophys. Res. 108 (B5), 2241. doi:10.1029/2002JB001866. Behncke, B., Neri, M., 2003. The July–August 2001 eruption of Mt. Etna (Sicily). Bull. Volcanol. 65, 461–476. doi:10.1007/s00445- 003-0274-1. Behncke, B., Neri, M., Pecora, E., Zanon, V., 2006. The exceptional activity and growth of the Southeast Crater, Mount Etna (Italy), between 1996 and 2001. Bull. Volcanol. doi:10.1007/s00445-006- 0061-x. Bonaccorso, A., 2001. Mt Etna volcano: modelling of ground deformation patterns of recent eruptions and considerations on the associated precursors, special number on “Mechanics and Thermalfluid Dynamics of the Volcanic Processes”. J. Volcanol. Geotherm. Res. 109, 99–108. Bonaccorso, A., Davis, P.M., 1999. Models of ground deformation from vertical volcanic conduits with application to eruptions of Mount, St. Helens and Mount Etna. J. Geophys. Res. 104, 10531–10542. Bonaccorso, A., Davis, P.M., 2004. Modeling of ground deformation associated with recent lateral eruptions: mechanics of magma ascent and intermediate storage at Mt. Etna. Monograph of American Geophysical Union “Etna: Volcano Laboratory”, vol. 143, pp. 293–306. Bonaccorso, A., Patanè, D., 2001. Shear response to an intrusive episode at Mt. Etna volcano (January 1998) inferred through seismic and tilt data. Tectonphysics 334, 61–75. Bonaccorso, A., Falzone, G., Raia, G., Villari, L., 1998. Application of new technology for ground deformation continuous detection. Acta Vulcanol. 10 (1), 7–12. Bonaccorso, A., Campisi, O., Falzone, G., Gambino, S., 2004. Continuous tiltmonitoring: a lesson from20 years experience at Mt. Etna. Monograph of American Geophysical Union “Etna: Volcano Laboratory”, vol. 143, pp. 307–320. Bonaccorso, A., Cianetti, S., Giunchi, C., Transatti, E., Bonafede, M., Boschi, E., 2005. Analytical and 3D numerical modeling of Mt. Etna (Italy) volcano inflation. Geophys. J. Int. 163, 852–862. Chiarabba, C., Amato, A., Boschi, E., Barberi, F., 2000. Recent seismicity and tomographic modeling of the Mt. Etna plumbing system. J. Geophys. Res. 108, 2556. doi:10.1029/2003JB002542. Corsaro, R., Pompilio, M., 2004a. Buoyancy-controlled eruption of magmas at Mt Etna. Terra Nova 16, 16–22. Corsaro, R., Pompilio, M., 2004b. Magma dynamics in the shallow plumbing system of Mt. Etna as recorded by compositional variations in volcanics of recent summit activity (1995–1999). J. Volcanol. Geotherm. Res. 137, 55–71. Davis, P.M., 1986. Surface deformation due to inflation of an arbitrarily oriented triaxial ellipsoidal cavity in an elastic half-space with reference to Kilauea volcano, Hawaii. J. Geophys. Res. 91, 7429–7430. Del Pezzo, E., De Martino, S., Gresta, S., Martini, M., Milana, G., Patanè, D., Sabbarese, C., 1993. Velocity and spectral characteristics of the volcanic tremor at Etna deduced by a small seismometer array. J. Geophys. Res. 56, 369–378. Dzurisin, D., 1992. Electronic tiltmeters for volcano monitoring: lessons from Mount St. Helens in Monitoring volcanoes: techniques and strategies by the staff of the Cascades observatory, 1980–90. In: Ewert, J.W., Swanson, D.A. (Eds.), U.S.G.S. Book, pp. 69–83. GVN, 1998. Global volcanism network. Bulletin of the Global Volcanism Program of the Smithsonian Institution, Washington DC, vol. 23. GVN, 2000. Global volcanism network. Bulletin of the Global Volcanism Program of the Smithsonian Institution, Washington DC, vol. 3. Harris, A.J.L., Neri, M., 2002. Volumetric observations during paroxysmal eruptions at Mount Etna: pressurized drainage of a shallow chamber or pulsed supply? J. Volcanol. Geotherm. Res. 116, 79–95. INGV-CT, Istituto Nazionale di Geofisica e Vulcanologia — Sezione di Catania, 2001. Multidisciplinary approach yields insight Mt. Etna eruption. Eos, Trans. AGU 82 (52), 653–656. Landau, L.D., Lifshitz, E.M., 1975. Theory of Elasticity, 2nd ed. Pergamon, Tarrytown, N.Y. La Delfa, S., Patanè, G., Clocchiatti, R., Joron, J.L., Tanguy, J.C., 2001. Activity preceding the February 1999 fissure eruption: inferred mechanism from seismological and geochemical data. J. Volcanol. Geotherm. Res. 105, 121–139. Lungarini, L., Troise, C., Meo, M., De Natale, G., 2005. Finite element modelling of topography effects on elastic on elastic ground deformation atMt Etna. J. Volcanol. Geotherm. Res. 144, 257–271. Marquardt, D.W., 1963. An algorithm for least estimation of non-linear parameters. J. Soc. Ind. Appl. Math. 11, 431–441. Métrich, N., Allard, P., Spilliaert, N., Andronico, D., Burton, M., 2004. 2001 flank eruption of the alkali- and volatile-rich primitive basalt responsible for Mount Etna's evolution in the last three decades. Earth Planet. Sci. Lett. 228, 1–17. Mogi, K., 1958. Relations between eruptions of various volcanoes and the deformations of the ground surfaces around them. Bull. Earthq. Res. Inst. Univ. Tokyo 36, 99. Okada, Y., 1985. Surface deformation due to shear and tensile faults in half-space. Bull. Seismol. Soc. Am. 75, 1135–1154. Patanè, D., Chiarabba, C., Cocina, O., De Gori, P., Moretti, M., Boschi, E., 2002. Tomographic images and 3D earthquakes locations of the seismic swarm preceding the 2001 Mt. Etna eruption: evidence for a dike intrusion. Geophys. Res. Lett. 29 (10). doi:10.1029/2001GLO14391. Patanè, D., De Gori, P., Chiarabba, C., Bonaccorso, A., 2003. Magma ascent and the pressurization of Mount Etna’s volcanic system. Science 299, 2061–2063. Polacci, M., Corsaro, R.A., Andronico, D., 2006. Coupled textural and compositional characterization of basaltic scoria: insights into the transition from Strombolian to fire fountain activity at Mount Etna, Italy. Geology 34, 201–204. Puglisi, G., Bonforte, A., 2004. Dynamics of Mt. Etna volcano inferred from static and kinematics GPS measurements. J. Geophys. Res. 109 (B11404). doi:10.1029/2003JB002878. Puglisi, G., Bonforte, A., Maugeri, S.R., 2001. Ground deformation patterns on Mt. Etna, 1992 to 1994, inferred from GPS data. Bull. Volcanol. 62, 371–384. Spilliaert, N., Allard, P., Métrich, N., Sobolev, A.V., 2006. Melt inclusion record of the conditions of ascent, degassing and extrusion of volatile-rich alkali basalt during the powerful 2002 flank eruption of Mount Etna (Italy). J. Geophys. Res. III, B04203. doi:10.1029/2005JB003934. Spilliaert, N., Métrich, N., Allard, P., in press. S–Cl–F degassing pattern of water-rich alkali basalt: modelling and relationship with eruption styles on Mount Etna. Earth Planet. Sci. Lett. Williams, C.A., Wadge, G., 1998. The effect of topography on magma chamber deformation models: application to Mt Etna radar interferometry. Geophys.Res.Lett. 25 (10), 1549–1552. Wyatt, F., 1988. Measurements of coseismic deformation in Southern California: 1972–1982. J. Geophys. Res. 93, 7923–7942.en
dc.description.fulltextreserveden
dc.contributor.authorBonaccorso, A.en
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italiaen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextrestricted-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia-
crisitem.author.orcid0000-0002-4770-6006-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent05. General-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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