Please use this identifier to cite or link to this item:
http://hdl.handle.net/2122/5223
DC Field | Value | Language |
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dc.contributor.authorall | Bonaccorso, A.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Catania, Catania, Italia | en |
dc.contributor.authorall | Bonforte, A.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Catania, Catania, Italia | en |
dc.contributor.authorall | Gambino, S.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Catania, Catania, Italia | en |
dc.contributor.authorall | Mattia, M.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Catania, Catania, Italia | en |
dc.contributor.authorall | Guglielmino, F.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Catania, Catania, Italia | en |
dc.contributor.authorall | Puglisi, G.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Catania, Catania, Italia | en |
dc.contributor.authorall | Boschi, E.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione AC, Roma, Italia | en |
dc.date.accessioned | 2009-10-30T07:09:44Z | en |
dc.date.available | 2009-10-30T07:09:44Z | en |
dc.date.issued | 2009-05-10 | en |
dc.identifier.uri | http://hdl.handle.net/2122/5223 | en |
dc.description.abstract | The multi-parametric permanent system (tilt and GPS networks, robotized geodetic station) for monitoring ground deformation at Stromboli volcano was set up in the 1990s and later greatly improved during the effusive event of 2002–2003. Unlike other volcanoes, e.g. Mt. Etna, the magnitude of ground deformation signals of Stromboli is very small and through the entire period of operation of the monitoring system, only two major episodes of deformation, in 1994–1995 and 2000, which did not lead to an eruption but rather pure intrusion, were measured. Similarly to the 2002–2003 eruption, no important deformations were detected in the months before the 2007 eruption. However, unlike the 2002–2003 eruption, GPS and tilt stations recorded a continuous deflation during the entire 2007 eruption, which allowed us to infer a vertical elongated prolate ellipsoidal source, centered below the summit craters at depth of about 2.8 km b.s.l. Due to its geometry and position, this source simulates an elongated plumbing system connecting the deeper LP magma storage (depth from 5 to 10 km) with the HP shallower storage (0.8–3 km), both previously identified by petrologic and geochemical studies. This result represents the first contribution of geophysics to the definition of the plumbing system of Stromboli at intermediate depth. Finally, no deformation due to the plumbing system was measured for a long time after the end of the eruption. Meanwhile, the new terrestrial geodetic monitoring system installed within the Sciara del Fuoco, on the lava fan formed during the eruption, indicated that during the first months after the end of the eruption the ground velocity progressively decreased in time, suggesting that part of the deformation was due to the thermal contraction of the lava flow. | en |
dc.language.iso | English | en |
dc.publisher.name | Elsevier | en |
dc.relation.ispartof | Journal of Volcanology and Geothermal Research | en |
dc.relation.ispartofseries | /182 (2009) | en |
dc.subject | Stromboli | en |
dc.subject | Ground Deformation | en |
dc.subject | source modelling | en |
dc.subject | flank instability | en |
dc.title | Insight on recent Stromboli eruption inferred from terrestrial and satellite ground deformation measurements | en |
dc.type | article | en |
dc.description.status | Published | en |
dc.type.QualityControl | Peer-reviewed | en |
dc.description.pagenumber | 172-181 | en |
dc.subject.INGV | 04. Solid Earth::04.03. Geodesy::04.03.06. Measurements and monitoring | en |
dc.subject.INGV | 04. Solid Earth::04.03. Geodesy::04.03.07. Satellite geodesy | en |
dc.subject.INGV | 04. Solid Earth::04.03. Geodesy::04.03.09. Instruments and techniques | en |
dc.subject.INGV | 04. Solid Earth::04.08. Volcanology::04.08.06. Volcano monitoring | en |
dc.subject.INGV | 04. Solid Earth::04.08. Volcanology::04.08.07. Instruments and techniques | en |
dc.subject.INGV | 04. Solid Earth::04.08. Volcanology::04.08.08. Volcanic risk | en |
dc.subject.INGV | 05. General::05.02. Data dissemination::05.02.03. Volcanic eruptions | en |
dc.identifier.doi | 10.1016/j.jvolgeores.2009.01.007 | en |
dc.relation.references | Barberi, F., Rosi, M., Sodi, A., 1993. Volcanic hazard assessment at Stromboli based on review of historical data. Acta Vulcanologica, 3: 173-187. Bertagnini, A., Métrich, N., Landi, P., Rosi, M., 2003. Stromboli volcano (Aeolian Archipelago, Italy): An open window on the deep-feeding system of a steady state basaltic volcano. J. Geophys. Res., 108(B7): 2336, doi:10.1029/2002JB002146. Bonaccorso, A., 1998. Evidence of a dyke-sheet intrusion at Stromboli volcano inferred through continuous tilt. Geophys. Res. Lett., 25 (22): 4225. Bonaccorso, A., Gambino, S., Guglielmino, F., Mattia, M., Puglisi, G., Boschi, E., 2008. Stromboli 2007 eruption : Deflation modeling to infer shallow-intermediate plumbing system. Geophys. Res. Lett., 35: doi:10.1029/2007GL032921. Burton, M.R., Allard, P., Muré, F., La Spina, A., 2007. Magmatic gas composition reveals the source depth of slug-driven Strombolian explosive activity. Science, 317: 227-230. Chouet, B., Saccorotti, G., Dawson, P., Martini, M., Scarpa, R., De Luca, G., Milana, G., Cattaneo, M., 1999. Broadband measurements of the sources of explosions at Stromboli Volcano, Italy. Geophys. Res. Lett., 28: 1937-1940. D’Auria L., Giudicepietro F., Martini M., Orazi M., 2007. The April-May 2006 volcano-tectonic events at Stromboli volcano (Southern Italy) and their relation with the magmatic system. Earth-prints Repository. http://hdl.handle.net/2122/1506. King R.W., Bock Y., 2000. Documentation for GAMIT GPS Analysis Software version 10.01. Massachusetts Institute of Technology and Scripts Institution of Oceanography, Cambridge Mass. Herring, T.A. (2000), GLOBK: Global Kalaman filter VLBI and GPS analysis program version 4.10, Mass. Inst. Of Technol., Cambridge, Mass. Landi P., Métrich, N., Bertagnini, A., Rosi, M., 2004. Dynamics of magma mixing and degassing recorded in plagioclase at Stromboli (Aeolian Archipelago, Italy). Contributions to Mineralogy and Petrology 147 (5): 629-631. Francalanci, L., Davies, G.R., Lustenhouwer, W., Tommasini, S., Mason, P.R.D., Conticelli, S., 2005. Intra-Grain Sr Isotope Evidence for Crystal Recycling and Multiple Magma Reservoirs in the Recent Activity of Stromboli Volcano, Southern Italy. J. Petrology, 46(10):1997-2021; doi:10.1093/petrology/egi045. Mattia, M., Rossi M., Guglielmino F., Aloisi M., Bock Y., 2004. The shallow plumbing system of Stromboli Island as imaged from 1 Hz instantaneous GPS positions. Geophysical Research Letters, 31: L24610, doi:10.1029/2004GL021281. Mattia M., Aloisi M., Di Grazia g., Gambino S., Palano M., Bruno V., 2008. Geophysical investigations of the plumbing system of Stromboli volcano (Aeolian Island, Italy). J. Volcanol. Geotherm. Res., doi: 10.1016/j.jvolgeres.2008.04.022. Nunnari G., Spata, A., Puglisi, G. A warning system for Stromboli volcano based on statistical analysis. Submittetd to Pure Appl. Geoph., J. I. Díaz, J. Fernandez, A. Camacho Eds. "Earth Sciences and Mathematics". Pasquarè, G., Francalanci, L., Garduno, V.H., Tibaldi, A., 1993. Structure and geologic evolution of the Stromboli volcano, Aeolian Islands, Italy. Acta Vulcanol., 3: 79-89. Patanè D., Mattia, M., Di Grazia, G., Cannavò, F., Giampiccolo, E., Musumeci, C., Montalto, P., Boschi E., 2007. Insights into the dynamical processes of the 2007 Stromboli eruption and possible meteorological influences on the magmatic system. Geophys. Res. Lett., 34: L22309, doi:10.1029/2007GL031730. Puglisi, G., Bonaccorso, A., Mattia, M., Aloisi, M., Bonforte, A., Campisi, O., Cantarero, M., Falzone, G., Puglisi, B., Rossi M., 2005. New integrated geodetic monitoring system at Stromboli volcano (Italy). Engineering Geology, 79: 13-31. Tibaldi A., 1996. Mutual influence of dyking and collapses at Stromboli volcano, Aeolian Arc, Italy. Volcano Instability. Spec. Publ., Geological Society of London 110: 55–63. Tibaldi A., 2001. Multiple sector collapses at Stromboli volcano, Italy: how they work. Bull. Volcanol., 63: 112-125. DOI 10.1007/s004450100129. | en |
dc.description.obiettivoSpecifico | 1.3. TTC - Sorveglianza geodetica delle aree vulcaniche attive | en |
dc.description.journalType | JCR Journal | en |
dc.description.fulltext | reserved | en |
dc.contributor.author | Bonaccorso, A. | en |
dc.contributor.author | Bonforte, A. | en |
dc.contributor.author | Gambino, S. | en |
dc.contributor.author | Mattia, M. | en |
dc.contributor.author | Guglielmino, F. | en |
dc.contributor.author | Puglisi, G. | en |
dc.contributor.author | Boschi, E. | en |
dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia | en |
dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia | en |
dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia | en |
dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia | en |
dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia | en |
dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia | en |
dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia, Sezione AC, Roma, Italia | en |
item.openairetype | article | - |
item.cerifentitytype | Publications | - |
item.languageiso639-1 | en | - |
item.grantfulltext | restricted | - |
item.openairecristype | http://purl.org/coar/resource_type/c_18cf | - |
item.fulltext | With Fulltext | - |
crisitem.author.dept | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia | - |
crisitem.author.dept | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia | - |
crisitem.author.dept | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia | - |
crisitem.author.dept | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia | - |
crisitem.author.dept | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia | - |
crisitem.author.dept | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia | - |
crisitem.author.orcid | 0000-0002-4770-6006 | - |
crisitem.author.orcid | 0000-0003-0435-7763 | - |
crisitem.author.orcid | 0000-0001-8055-3059 | - |
crisitem.author.orcid | 0000-0001-6220-4947 | - |
crisitem.author.orcid | 0000-0003-3258-9975 | - |
crisitem.author.orcid | 0000-0003-4503-5808 | - |
crisitem.author.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
crisitem.author.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
crisitem.author.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
crisitem.author.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
crisitem.author.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
crisitem.author.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
crisitem.classification.parent | 04. Solid Earth | - |
crisitem.classification.parent | 04. Solid Earth | - |
crisitem.classification.parent | 04. Solid Earth | - |
crisitem.classification.parent | 04. Solid Earth | - |
crisitem.classification.parent | 04. Solid Earth | - |
crisitem.classification.parent | 04. Solid Earth | - |
crisitem.classification.parent | 05. General | - |
crisitem.department.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
crisitem.department.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
crisitem.department.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
crisitem.department.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
crisitem.department.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
crisitem.department.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
crisitem.department.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
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Bonaccorso_et_al-JVGR-2009.pdf | 2.57 MB | Adobe PDF |
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