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  • Stromboli  (8)
  • Crustal deformation (cf. Earthquake precursor: deformation or strain)  (7)
  • 1
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    Analytical and 3-D numerical modelling of Mt. Etna (Italy) volcano inflation (2005)
    In:  Geophys. J. Int., Taipei, Elsevier, vol. 163, no. 2, pp. 852-862, pp. 2091, (ISBN: 0-12-018847-3)
    Details
    Publication Date: 2005
    Keywords: Modelling ; Three dimensional ; Volcanology ; Crustal deformation (cf. Earthquake precursor: deformation or strain) ; Geodesy ; Inversion ; Davis ; Yang ; Finite Element Method ; Inhomogeneity ; GJI ; finite-element ; methods, ; lateral ; heterogeneity, ; volcanic ; activity, ; structure
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    BIBLIOGRAPHY SEISMOLOGY
  • 2
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    Plate motion and dragging of the upper mantle: Lateral variations of lithospheric thickness and their implications for intraplate deformation (1992)
    In:  Geophys. Res. Lett., Basel, Inst. f. Geophys., Ruhr-Univ. Bochum, vol. 19, no. 4, pp. 749-752, pp. 1417, (ISSN: 1340-4202)
    Details
    Publication Date: 1992
    Keywords: Plate tectonics ; Crustal deformation (cf. Earthquake precursor: deformation or strain) ; earth mantle ; ConvolutionE ; GRL
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    BIBLIOGRAPHY SEISMOLOGY
  • 3
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    Global postseismic gravity changes of a viscoelastic Earth (1998)
    In:  Journal of Geophysical Research, Warszawa, Polish Geothermal Association, vol. 103, no. B12, pp. 29867-29885, pp. B05406, (ISSN: 1340-4202)
    Details
    Publication Date: 1998
    Keywords: Inelastic ; Rheology ; Crustal deformation (cf. Earthquake precursor: deformation or strain) ; Gravimetry, Gravitation ; JGR
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    BIBLIOGRAPHY SEISMOLOGY
  • 4
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    Global postseismic deformation in a stratified viscoelastic Earth: effects on Chandler wobble excitation (1983)
    In:  J. Geophys. Res., Luxembourg, Conseil de l'Europe, vol. 88, no. B9, pp. 2240-2250, pp. B09201, (ISBN 1-86239-117-3)
    Details
    Publication Date: 1983
    Keywords: Crustal deformation (cf. Earthquake precursor: deformation or strain) ; Inelastic ; Layers ; Chandler wobble ; JGR
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    BIBLIOGRAPHY SEISMOLOGY
  • 5
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    Seismic deformation in the Mediterranean area estimated by moment tensor summation (1995)
    In:  Geophys. J. Int., Stockholm, Wissenschaftliche Buchgesellschaft, vol. 122, no. 1-2, pp. 938-952, pp. L15318, (ISSN: 1340-4202)
    Details
    Publication Date: 1995
    Keywords: Moment tensor ; Seismicity ; Tectonics ; Crustal deformation (cf. Earthquake precursor: deformation or strain) ; GJI
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    BIBLIOGRAPHY SEISMOLOGY
  • 6
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    The September 26, 1997, Colfiorito, Italy, earthquakes: Modeled coseismic surface displacement from SAR interferometry and Global Positioning System (1999)
    In:  Geophysical Research Letters, Leyden, Noordhoff International Publishing, vol. 26, no. 7, pp. 883-886, pp. B04306, (ISSN: 1340-4202)
    Details
    Publication Date: 1999
    Keywords: Earthquake ; Crustal deformation (cf. Earthquake precursor: deformation or strain) ; Geodesy ; InSAR ; GRL
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    BIBLIOGRAPHY SEISMOLOGY
  • 7
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    Recent Evolution and Seismicity of the Mediterranean Region (1993)
    Kluwer Acad. Publ.
    In:  Dordrecht, Kluwer Acad. Publ., vol. 70, pp. 158, (ISBN 3-9808780-0-7)
    Details
    Publication Date: 1993
    Keywords: Tectonics ; Seismicity ; Greece ; Crustal deformation (cf. Earthquake precursor: deformation or strain) ; Geol. aspects ; Plate tectonics
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    BIBLIOGRAPHY SEISMOLOGY
  • 8
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    Insight on recent Stromboli eruption inferred from terrestrial and satellite ground deformation measurements (2009)
    Elsevier
    Details
    Publication Date: 2017-04-04
    Description: 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.
    Description: Published
    Description: 172-181
    Description: 1.3. TTC - Sorveglianza geodetica delle aree vulcaniche attive
    Description: JCR Journal
    Description: reserved
    Keywords: Stromboli ; Ground Deformation ; source modelling ; flank instability ; 04. Solid Earth::04.03. Geodesy::04.03.06. Measurements and monitoring ; 04. Solid Earth::04.03. Geodesy::04.03.07. Satellite geodesy ; 04. Solid Earth::04.03. Geodesy::04.03.09. Instruments and techniques ; 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::05.02. Data dissemination::05.02.03. Volcanic eruptions
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 9
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    Stromboli: a natural laboratory of environmental science (2008)
    Elsevier
    Details
    Publication Date: 2017-04-04
    Description: The science of environment is per se multi- and inter-disciplinary. It is not possible to separate the role of the physical, chemical, biological, and anthropic factors, respectively. Research must therefore rely on suitable natural laboratories, where all different effects can be simultaneously monitored and investigated. Stromboli is a volcanic island slightly North of Sicily, within a tectonic setting characterised by a Benioff zone, curved like a Greek theatre, opened towards the Tyrrhenian Sea, with deep earthquakes. Moreover, it is a unique volcano in the world in that since at least ~ 3000 years ago, it has exploded very regularly, about every 15^20 min. Hence, it is possible to monitor statistically phenomena occurring prior, during, and after every explosion. The Istituto Nazionale di Geofisica e Vulcanologia (INGV) has recently established a permanent Laboratory and an extensive interdisciplinary programme is being planned. A few main classes of items are to be considered including: (1) matter exchange (solid, liquid, gas, chemistry); (2) thermal and/or radiative coupling; (3) electromagnetic coupling; (4) deformation; (5) biospheric implications; and (6) anthropic relations since either the times of the Neolithic Revolution. Such an entire multidisciplinary perspective is discussed, being much beyond a mere volcanological concern. We present here the great heuristic potential of such a unique facility, much like a natural laboratory devoted to the investigation of the environment and climate.
    Description: Published
    Description: 429-442
    Description: JCR Journal
    Description: reserved
    Keywords: Stromboli ; natural laboratory ; environmental science ; 04. Solid Earth::04.02. Exploration geophysics::04.02.99. General or miscellaneous ; 04. Solid Earth::04.05. Geomagnetism::04.05.04. Magnetic anomalies ; 05. General::05.04. Instrumentation and techniques of general interest::05.04.99. General or miscellaneous
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 10
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    The 2007 Stromboli eruption: event chronology and effusion rates using thermal infrared data (2009)
    American Geophysical Union
    Details
    Publication Date: 2017-04-04
    Description: Accepted for publication in Journal of Geophysical Research. Copyright (2009) American Geophysical Union. Further reproduction or electronic distribution is not permitted.
    Description: Using thermal infrared images recorded by a permanent thermal camera network maintained on Stromboli volcano (Italy), together with satellite and helicopter-based thermal image surveys, we have compiled a chronology of the events and processes occurring before and during Stromboli’s 2007 effusive eruption. These digital data also allow us to calculate the effusion rates and lava volumes erupted during the effusive episode. At the onset of the 2007 eruption, two parallel eruptive fissures developed within the North East crater, eventually breaching the NE flank of the summit cone and extending along the eastern margin of the Sciara del Fuoco. These fed a main effusive vent at 400 m a.s.l. to feed lava flows that extended to the sea. The effusive eruption was punctuated, on 15 March, by a paroxysm with features similar to the 5 April paroxysm that occurred during the 2002-03 effusive eruption. A total of between 3.2 x 106 m3 and 11 x 106 m3 of lava was erupted during the 2007 eruption over 34 days of effusive activity. More than half of this volume was emplaced during the first 5.5 days of the eruption. Although the 2007 effusive eruption had a comparable erupted volume to the previous (2002-03) effusive eruption, it had a shorter duration and thus a mean output rate (= total volume divided by eruption duration) that was one order of magnitude greater than the 2002-03 event (~2.4 m3 s-1 compared with 0.32±0.28 m3 s-1). In this paper, we discuss similarities and differences between these two effusive events, and interpret the processes occurring in 2007 in terms of the recent dynamics witnessed at Stromboli.
    Description: This paper was partially supported by a grant to S. Calvari (Project INGV-DPC Paroxysm V2/03, 2008-2010) funded by the Istituto Nazionale di Geofisica e Vulcanologia and by the Italian Civil Protection. Satellite-based effusion rate work by A. Steffke and A. Harris was supported by NASA grant NNG04GO64G "New Tools for Advanced Hot Spot Tracking".
    Description: In press
    Description: 1.5. TTC - Sorveglianza dell'attività eruttiva dei vulcani
    Description: JCR Journal
    Description: open
    Keywords: Thermal mapping ; Stromboli ; 04. Solid Earth::04.08. Volcanology::04.08.06. Volcano monitoring
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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