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Magma dynamics during the 2007 Stromboli eruption (Aeolian Islands. Italy): mineralogical, geochemical and isotopic data
Author(s)
Language
English
Obiettivo Specifico
Status
Published
JCR Journal
JCR Journal
Peer review journal
Yes
Title of the book
Issue/vol(year)
/182(2009)
Publisher
Elsevier
Pages (printed)
255–268
Issued date
November 2009
Last version
http://hdl.handle.net/2122/4548
Abstract
After the 6 month-long effusive event of 2002-2003, a new lava effusion occurred at Stromboli between 27
February and 2 April 2007. Despite the different durations, approximately the same volume of magma was
emitted in both eruptions, in the order of 107
m3
. A paroxysmal eruption occurred at the summit craters in
both the 2002–2003 and 2007 episodes, during which a significant amount of low porphyritic (LP), volatile-
rich magma was erupted. In both cases, the paroxysm did not interrupt the lava emission. Here, we present
compositional data, including texture, mineralogy, chemistry and Sr and Nd isotope ratios of bulk-rock,
groundmass and separated minerals of lavas erupted in 2007, together with chemistry and Sr and Nd isotope
composition of the pumices emitted during the 15 March paroxysm. As a whole, the lavas have the same
texture and chemistry that characterize the highly porphyritic (HP) products usually erupted at Stromboli
during normal Strombolian activity and effusive events. Compared to the previous HP products, the 2007
lavas show minor but systematic mineralogical and isotopic variations which are consistent with a modest
increase of the magma supply rate of the volcano. Compositional variations during the entire duration of the
event are very modest. Glass chemistry changes in lavas erupted in the second half of March can be explained
by theminormixing between the volatile-rich LPmagma rising through the shallowmagmatic systemduring the
15 March paroxysm and the degassed residing HP magma. A first conclusion of this study is that there is no
compositional evidence supporting major changes in the magma dynamics of the volcano accompanying the
effusive activity, as also suggested for the 2002–2003 event. The activity of Stromboli is controlled by a steady
state feeding system in which refilling, mixing, degassing and crystallization at shallow level continuously
operate,withmodest oscillations in themagma supply rate. Switching between normal Strombolian and effusive
activity is related to periods of relatively more vigorous refilling of the shallow system, leading to progressive
pressure increase in the upper conduits associated with only minor compositional variations in the erupted
products.
February and 2 April 2007. Despite the different durations, approximately the same volume of magma was
emitted in both eruptions, in the order of 107
m3
. A paroxysmal eruption occurred at the summit craters in
both the 2002–2003 and 2007 episodes, during which a significant amount of low porphyritic (LP), volatile-
rich magma was erupted. In both cases, the paroxysm did not interrupt the lava emission. Here, we present
compositional data, including texture, mineralogy, chemistry and Sr and Nd isotope ratios of bulk-rock,
groundmass and separated minerals of lavas erupted in 2007, together with chemistry and Sr and Nd isotope
composition of the pumices emitted during the 15 March paroxysm. As a whole, the lavas have the same
texture and chemistry that characterize the highly porphyritic (HP) products usually erupted at Stromboli
during normal Strombolian activity and effusive events. Compared to the previous HP products, the 2007
lavas show minor but systematic mineralogical and isotopic variations which are consistent with a modest
increase of the magma supply rate of the volcano. Compositional variations during the entire duration of the
event are very modest. Glass chemistry changes in lavas erupted in the second half of March can be explained
by theminormixing between the volatile-rich LPmagma rising through the shallowmagmatic systemduring the
15 March paroxysm and the degassed residing HP magma. A first conclusion of this study is that there is no
compositional evidence supporting major changes in the magma dynamics of the volcano accompanying the
effusive activity, as also suggested for the 2002–2003 event. The activity of Stromboli is controlled by a steady
state feeding system in which refilling, mixing, degassing and crystallization at shallow level continuously
operate,withmodest oscillations in themagma supply rate. Switching between normal Strombolian and effusive
activity is related to periods of relatively more vigorous refilling of the shallow system, leading to progressive
pressure increase in the upper conduits associated with only minor compositional variations in the erupted
products.
References
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explosive eruptions at Stromboli volcano using multidisciplinary data: an example
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Baldi, P., Coltelli, M., Fabris, M., Marsella, M., Tommasi, P., 2008. High precision photo-
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2002 flank failure and tsunami at Stromboli volcano inferred by volcanological and
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short magma residence time for the 20th century activity at Stromboli volcano,
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measurement of the volcanic gas plume CO2/SO2 ratio. J. Volcanol. Geoth. Res. 182,
221–230 (this issue).
Allard, P., Carbonnelle, J., Métrich, N., Loyer, H., Zettwoog, P., 1994. Sulphur output and
magma degassing budget of Stromboli volcano. Nature 368, 326–330.
Andronico, D., Corsaro, R.A., Cristaldi, A., Polacci, M., 2008. Characterizing high energy
explosive eruptions at Stromboli volcano using multidisciplinary data: an example
from the 9 January 2005 explosion. J. Volcanol. Geotherm. Res. 176, 541–550.
doi:10.1016/j.jvolgeores.2008.05.011.
Armienti, A., Francalanci, L., Landi, P., 2007. Textural effects of steady state behaviour of
the Stromboli feeding system. J. Volcanol. Geoth. Res. 160, 86–98.
Avanzinelli, R., Boari, E., Conticelli, S., Francalanci, L., Gualtieri, L., Perini, G., Petrone, C.M.,
Tommasini, S., Ulivi, M., 2005. High precision Sr, Nd, and Pb isotopic analyses using
new generation Thermal Ionisation Mass Spectrometer ThermoFinnigan Triton-Ti
®.
Period. Mineral. 74 (3), 147–166.
Baldi, P., Coltelli, M., Fabris, M., Marsella, M., Tommasi, P., 2008. High precision photo-
grammetry formonitoring the evolution of the NWflank of Stromboli volcano during and
after the 2002–2003 eruption. Bull. Volcanol. 70, 703–715. doi:10.1007/s00445-007-
0162-1.
Barberi, F.,Rosi,M., Sodi,A.,1993.Volcanichazard assessment at Stromboli based onreview
of historical data. Acta Vulcanol. 3, 173–187.
Bertagnini, A., Coltelli,M., Landi, P., Pompilio,M., Rosi,M., 1999. Violent explosions yield
new insights into dynamics of Stromboli volcano. EOS 80, 635–636.
Bertagnini, A., Métrich, N., Landi, P., Rosi, M., 2003. Stromboli an open window on the
deep feeding system of a steady state volcano. J. Geophys. Res. 108 (B7), 2336.
doi:10,1029/2002JB002146.
Bertagnini, A., Métrich, N., Francalanci, L., Landi, P., Tommasini, S., Conticelli, S., 2008.
Volcanology and Magma Geochemistry of the Present-day Activity: Constraints on
the Feeding System. In: “Learning from Stromboli and its 2002–2003 Eruptive
Crisis”, Calvari, S., Rosi, M., and Ripepe, M. (edts), American Geophysical Union –
Geophysical Monograph volume.
Bonaccorso, A., Cardaci, C., Coltelli, M., Del Carlo, P., Falsaperla, S., Panucci, S., Pompilio,M.,
Villari, L.,1996. Annual report of theworld volcanic eruptions in 1993, Stromboli. Bull.
Volcan. Eruptions 33, 7–13.
Bonaccorso, A., Calvari, S., Garfi, G., Lodato, L., Patane, D., 2003. Dynamics of the December
2002 flank failure and tsunami at Stromboli volcano inferred by volcanological and
geophysical observations. Geophys. Res. Lett. 30 (18). doi:10.1029/2003GL017702.
Bonaccorso, A., Gambino, S., Guglielmino, F., Mattia, M., Pugliesi, G., Boschi, E., 2008.
Stromboli 2007 eruption: deflection modeling to infer shallow-intermediate
plumbing system. Geophys. Res. Lett. 35, L06311. doi:10.1029/2007GL032921.
Calvari,S.,Spampinato,L.,Lodato,L.,Harris,A.J.L.,Patrick,A.R.,Dehn,J.,Burton,M.R.,Andronico,
D., 2005. Chronology and complex volcanic processes during the 2002-2003 flank
eruption at Stromboli volcano (Italy) reconstructed from direct observations and surveys
withahandheldthermalcamera.J.Geophys.Res.110. doi:10.1029/2004JB003129.
Calvari, S., Rosi,M., Ripepe,M., 2008. Learning fromStromboli and its 2002-2003 Eruptive
Crisis”. American Geophysical Union – Geophysical Monograph volume.
Capaldi, G., Guerra, I., Lo Bascio, A., Luongo, G., Pece, R., Rapolla, A., Scarpa, R., Del Pezzo,
E., Martini, M., Ghiara, M.R., Lirer, L., Munno, R., La Volpe, L., 1978. Stromboli and its
1975 eruption. Bull. Volcanol. 41, 259–285.
Carapezza, M.L., Ingaggiato, S., Brusca, L., Longo, M., 2004. Geochemical precursors of
the activity of an open-conduit volcano: the Stromboli 2002–2003 eruptive event.
Geophys. Res. Lett. 31, L07620. doi:10.1029/2004GL019614.
Corsaro, R.A., Pompilio, M., 2004. 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.
Corsaro, R.A., Miraglia, L., 2005. Composizione dei vetri dei prodotti emessi dallo
Stromboli nel periodo ottobre 2004-gennaio 2005. Report n. UFVG2005/008, INGV,
Sezione di Catania, Italy.
D 'Auria, F., Giudicepietro, F., Martini, M., Orazi, M., 2006. The April-May-2006 volcano
tectonic events at Stromboli volcano (southern Italy) and their relation with the
magmatic system. Earth Prints Repository. Istituto Nazionale di Geofisica e
Vulcanologia, Rome. http://hdl.handle.net/2122/1506.
De Fino, M., La Volpe, L., Falsaperla, S., Frazzetta, G., Neri, G., Francalanci, L., Rosi, M.,
Sbrana, A., 1988. The Stromboli eruption of December 6, 1985–April 25, 1986:
volcanological, petrological and seismological data. Rend. Soc. ital. Mineral. Pet. 43,
1021–1038.
Di Carlo, I., Pichavant, M., Rotolo, S., Scaillet, B., 2006. Experimental crystallization of a
High-K Arc Basalt: the Golden Pumice, Stromboli Volcano (Italy). J. Petrol. 1–27.
doi:10.1093/petrology/egl011.
Francalanci, L., Manetti, P., Peccerillo, A., 1989. Volcanological and magmatological
evolution of Stromboli volcano (Aeolian islands): the roles of fractional crystal-
lisation, magma mixing, crustal contamination and source heterogeneity. Bull.
Volcanol. 51, 355–378.
Francalanci, L., Tommasini, S., Conticelli, S., Davies, G.R., 1999. Sr isotope evidence for
short magma residence time for the 20th century activity at Stromboli volcano,
Italy. Earth Planet. Sci. Lett. 167, 61–69.
Francalanci, L., Tommasini, S., Conticelli, S., 2004. The volcanic activity of Stromboli in
the 1906-1998 period: mineralogical, geochemical and isotope data relevant to the
understanding of Strombolian activity. J. Volcanol. Geotherm. Res. 131, 179–211.
Francalanci, L., Davies, G.R., Lustenmhower, W., Tommasini, S., Mason, P.R.D., Conticelli,
S., 2005. Intra-grain Sr isotope evidence for crystal re-cycling and multiple magma
reservoirs in the recent activity of Stromboli volcano, Southern Italy. J. Petrol. 46,
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