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Curie isotherm depth from aeromagnetic data constraining shallow heat source depths in the central Aeolian Ridge (Southern Tyrrhenian Sea, Italy)
Author(s)
Language
English
Obiettivo Specifico
1.10. TTC - Telerilevamento
3.3. Geodinamica e struttura dell'interno della Terra
3.4. Geomagnetismo
3.6. Fisica del vulcanismo
5.4. Banche dati di geomagnetismo, aeronomia, clima e ambiente
Status
Published
JCR Journal
JCR Journal
Peer review journal
Yes
Title of the book
Issue/vol(year)
/75(2013)
Electronic ISSN
1432-0819
Publisher
Springer
Pages (printed)
article 710
Issued date
March 20, 2013
Subjects
Abstract
The Salina, Lipari, and Vulcano volcanic ridge
and the surrounding sea sectors (Aeolian Archipelago,
Southern Tyrrhenian Sea, Italy) are characterized by vents
responsible for a recent (<40 ka—1889/1890 AD) effusive
and explosive subareal activity and repeated, 56 to 7 ka in
age, submarine explosive eruptions from source areas located
between Lipari and Vulcano. A spectral depth estimation of
the magnetic bottom using a fractal method on aeromagnetic
data from Vulcano, Lipari, and Salina volcanic ridge allows us
to constrain the Curie isotherm depth. The elevated portion of
the isotherm is between 2 and 3 km below Salina and Vulcano
and about 1 km below Lipari. The Curie depth results in the
context of other geological and geophysical evidence suggest
that the rise of the Curie isotherm is mainly due to the
occurrence of shallow heat sources such as magma ponds
and associated hydrothermal systems. The short-wavelength
magnetic anomaly field reflects magnetic contrasts from
highly magnetized volcanic bodies, low-magnetization
sediments, and hydrothermally altered rocks. Borehole temperature
data verify the Curie temperature derived from the
magnetic methods on the island of Vulcano.We conclude that
the whole Vulcano, Lipari, and Salina volcanic ridge is active
and should be monitored.
and the surrounding sea sectors (Aeolian Archipelago,
Southern Tyrrhenian Sea, Italy) are characterized by vents
responsible for a recent (<40 ka—1889/1890 AD) effusive
and explosive subareal activity and repeated, 56 to 7 ka in
age, submarine explosive eruptions from source areas located
between Lipari and Vulcano. A spectral depth estimation of
the magnetic bottom using a fractal method on aeromagnetic
data from Vulcano, Lipari, and Salina volcanic ridge allows us
to constrain the Curie isotherm depth. The elevated portion of
the isotherm is between 2 and 3 km below Salina and Vulcano
and about 1 km below Lipari. The Curie depth results in the
context of other geological and geophysical evidence suggest
that the rise of the Curie isotherm is mainly due to the
occurrence of shallow heat sources such as magma ponds
and associated hydrothermal systems. The short-wavelength
magnetic anomaly field reflects magnetic contrasts from
highly magnetized volcanic bodies, low-magnetization
sediments, and hydrothermally altered rocks. Borehole temperature
data verify the Curie temperature derived from the
magnetic methods on the island of Vulcano.We conclude that
the whole Vulcano, Lipari, and Salina volcanic ridge is active
and should be monitored.
Sponsors
INGV
References
Aydın I, Karat HI, Koçak A (2005) Curie-point depth map of Turkey.
Geophys J Intern 162:633–640
Bansal AR, Gabriel G, Dimri VP, Krawczyk CM (2011) Estimation of
depth to the bottom of magnetic sources by a modified centroid
method for fractal distribution of sources: an application to
aeromagnetic data in Germany. Geophysics 76:L11–L22
Baranov V, Naudy H (1964) Numerical calculation of the formula of
reduction to the magnetic pole. Geophysics 29:67–79
Barberi F, Gandino A, Gioncada A, La Torre P, Sbrana A, Zenucchini
C (1994) The deep structure of the Eolian arc (Filicudi–Panarea–
Vulcano sector) in light of gravity, magnetic and volcanological
data. J Volcanol Geotherm Res 61:189–206
Blanco Montenegro I, De Ritis R, Chiappini M (2007) Imaging and
modelling the subsurface structure of volcanic calderas with highresolution
aeromagnetic data at Vulcano (Aeolian Islands, Italy).
Bull Volcanol 69(6):643–659. doi:10.1007/s00445-006-0100-7
Bouligand C, Glen JMG, Blakely RJ (2009) Mapping Curie temperature
depth in the western United States with a fractal model for
crustal magnetization. J Geophys Res 114:B11104. doi:10.1029/
2009JB006494
Boyce A (2007) Fluids in early stage hydrothermal alteration of highsulfidation
epithermal systems: a view from the Vulcano active
hydrothermal system (Aeolian Island, Italy). J Volcanol Geotherm
Res 166(2):76–90
Bruno PP, Paoletti V, Grimaldi M, Rapolla A (2000) Geophysical
exploration for geothermal low enthalpy resources in Lipari
Island, Italy. J Volcanol Geotherm Res 98:173–188
710, Page 10 of 11 Bull Volcanol (2013) 75:710
Chiappini M, Ferraccioli F, Bozzo E, Damaske D (2002) Regional
compilation and analysis of aeromagnetic anomalies for the
Transantarctic Mountains–Ross Sea sector of the Antarctic.
Tectonophysics 347:121–137
Castello B, Selvaggi G, Chiarabba C, Amato A (2005) Catalogo della
sismicità Italiana—CSI 10, 1981–2002, Cent Naz Terremoti, Ist
Naz di Geofis e. Vulcanol, Rome
Cicchino AMP, Zanella E, De Astis G, Lanza R, Lucchi F, Tranne CA,
Airoldi G, Mana S (2011) Rock magnetism and compositional
investigation of Brown Tuffs deposits at Lipari and Vulcano
(Aeolian Islands—Italy). J Volcanol Geotherm Res 208:23–38.
doi:10.1016/jjvolgeores201108007
De Astis G, Ventura G, Vilardo G (2003) Geodynamic significance of
the Aeolian volcanism (Southern Tyrrhenian Sea, Italy) in light of
structural, seismological and geochemical data. Tectonics
22:1040. doi:10.1029/2003TC001506
De Ritis R, Blanco-Montenegro I, Ventura G, Chiappini M (2005)
Aeromagnetic data provide new insights on the volcanism and
tectonics of Vulcano Island and offshore areas (southern
Tyrrhenian Sea, Italy). Geophys Res Lett 32:L15305. doi:10.1029/
2005GL023465
De Ritis R, Ventura G, Chiappini M (2007) Aeromagnetic anomalies
reveal hidden tectonic and volcanic structures in the central sector
of the Aeolian Islands, southern Tyrrhenian Sea, Italy. J Geophys
Res 112:B10. doi:10.1029/2006JB004639
De Rosa R, Guillou H, Mazzuoli R, Ventura G (2003a) New unspiked
K–Ar ages of volcanic rocks of the central and western sector of
the Aeolian Islands: reconstruction of the volcanic stages. J
Volcanol Geotherm Res 120:161–178
De Rosa R, Donato P, Gioncada A, Masetti M, Santacroce R (2003b)
The Monte Guardia eruption (Lipari, Aeolian Islands): an example
of reversely zoned magma mixing sequence. Bull Volcanol
65:530–543
Di Martino C, Frezzotti M, Lucchi F, Peccerillo A, Tranne C, Diamond
LW (2010) Magma storage and ascent at Lipari Island (Aeolian
Archipelago, Southern Italy) at 223–81 ka: the role of crustal
processes and tectonic influence. Bull Volcanol 72(9):1061–1076
Donato P, Behrens H, De Rosa R, Holtz F, Parat F (2006) Crystallization
conditions in Upper Pollara (Salina Island, Southern Tyrrhenian
Sea) magma chamber. Mineral Petrol 86:89–108
Faraone D, Silvano A, Verdiani G (1986) The monzogabbroic intrusion
in the island of Vulcano, Aeolian Archipelago, Italy. Bull
Volcanol 48:299–307
Fedi M, Quarta T, de Santis A (1997) Inherent power-law behavior of
magnetic field power spectra from a Spector and Grant ensemble.
Geophysics 62:1143–1150
Ferrucci F, Gaudiosi G, Milano G, Nercessian A, Vilardo G, Luongo G
(1991) Seismological exploration of Vulcano (Aeolian Islands,
Southern Tyrrhenian Sea): case history. Acta Vulcanol 1:143–152
Finn C, Sisson TW, Deszcz-Pan M (2001) Aerogeophysical measurements
of collapse–prone hydrothermally altered zones at Mount
Rainer volcano. Nature 409:600–603
Frezzotti ML, Peccerillo A, Bonelli R (2003) Magma ascent rates and
depths of magma reservoirs beneath the Aeolian volcanic arc
(Italy): inferences from fluid and melt inclusions in crustal xenoliths.
In: Bodnar B, De Vivo B (eds) Melt inclusions in volcanic
systems. Elsevier, Amsterdam, pp 185–206
Gambino S, Milluzzo V, Scaltrito A, Scarfì L (2012) Relocation and
focal mechanisms of earthquakes in the south-central sector of the
Aeolian Archipelago: new structural and volcanological insights.
Tectonophysics 524/525:108–115. doi:10.1016/jtecto201112024
Granieri D, Carapezza ML, Chiodini G (2006) Correlated increase in
CO2 fumarolic content and diffuse emission from La Fossa crater
(Vulcano, Italy): evidence of volcanic unrest or increasing gas
release from a stationary deep magma body? Geophys Res Lett
33:L13316. doi:10.1029/2006GL026460
Gvirtzman Z, Nur A (2001) Residual topography, lithospheric thickness,
and sunken slabs in the central Mediterranean. Earth Planet
Sci Lett 187:117–130
Lucchi F, Tranne CA, De Astis G, Keller J, Losito R, MorcheW(2008)
Stratigraphy and significance of Brown Tuffs of the Aeolian
Islands (southern Italy). J Volcanol Geotherm Res 117:49–70
Macmillan S, Maus D (2005) International geomagnetic reference
field—the tenth generation. Earth Planets Space 57:1135–1140
Maus S, Gordon D, Fairhead D (1997) Curie-temperature depth estimation
using a self-similar magnetization model. Geophys J
Intern 129:163–168. doi:10.1111/j1365-246X1997tb00945x
Maus S, Dimri VP (1996) Depth estimation from the scaling power
spectrum of potential fields? Geophys J Int 124:113–120
Mazzuoli R, Tortorici L, Ventura G (1995) Oblique rifting in Salina,
Lipari and Vulcano islands (Aeolian Islands, southern Italy). Terra
Nova 7:444–452
Nuccio PM, Paonita A (2001) Magmatic degassing of multicomponent
vapors and assessment of magma depth: application to Vulcano
Island (Italy). Earth Planet Sci Lett 193(3–4):467–481
Okubo Y, Graf RJ, Hansen RO, Ogawa K, Tsu H (1985) Curie-point
depths of the island of Kyushu and surrounding areas, Japan.
Geophysics 50:481–494
Pasquale V, Verdoya M, Chiozzi P (2003) Heat-flux budget in the
southeastern continental margin of the Tyrrhenian basin. Phys
Chem Earth 28:407–420
Peccerillo A, Frezzotti ML, De Astis G, Ventura G (2006) Modeling
the magma plumbing system of Vulcano (Aeolian Islands, Italy)
by integrated fluid-inclusion geobarometry, petrology, and
geophysics. Geology 34:17–20
Pilkington M, Todoeschuck JP (1993) Fractal magnetization of
continental crust. Geophys Res Lett 20:627–630
Ravat D, Salem A, Abdelaziz AMS, Elawadi E, Morgan P (2011)
Probing magnetic bottom and crustal temperature variations along
the Red Sea margin of Egypt. Tectonophysics 510:337–344
Ravat D, Pignatelli A, Nicolosi I, Chiappini M (2007) A study of spectral
methods of estimating the depth to the bottom of magnetic sources
from near-surface magnetic anomaly data. Geophys J Int 169:421–434
Romagnoli C, Calanchi N, Gabbianelli G, Lanzafame G, Rossi PL
(1989) Contributi delle ricerche di geologia marina alla
caratterizzazione morfostrutturale ed evolutiva dei complessi
vulcanici di Salina, Lipari e Vulcano (Isole Eolie). Boll Gruppo
Nazionale Vulcanologia 1989:971–978 (in italian)
Spector A, Grant FS (1970) Statistical models for interpreting
aeromagnetic data. Geophysics 35:293–302
Tanaka A, Okubo Y, Matsubayashi O (1999) Curie point depth based
on spectrum analysis of the magnetic anomaly data in East and
Southeast Asia. Tectonophysics 306:461–470
Tranne CA, Lucchi F, Calanchi N, Lanzafame G, Rossi PL (2002)
Geological map of the Island of Lipari (Aeolian Islands), scale
1:10000. University of Bologna and INGV, LAC Firenze
Ventura G, Vilardo G, Milano G, Pino NA (1999) Relationships among
crustal structure, volcanism and strike–slip tectonics in the Lipari–
Vulcano volcanic complex (Aeolian Islands, Southern Tyrrhenian
Sea, Italy). Phys Earth Planet Inter 116(1–4):31–52
Wang C, Hwang W, Shi Y (1989) Thermal evolution of a rift basin: the
Tyrrhenian Sea. J Geophys Res 94(B4):3991–4006
Zanella E, Lanza R (1994) Remanent and induced magnetization in the
volcanites of Lipari and Vulcano (Aeolian Islands). Annals
Geophys 37:1149–1156
Zanon V, Frezzotti ML, Peccerillo A (2003) Magmatic feeding system
and crustal magma accumulation beneath Vulcano Island (Italy):
evidence from CO2 fluid inclusions in quartz xenoliths. J
Geophys Res 108:2298–2301. doi:10.1029/2002JB002140
Zanon V, Nikogosian IK (2004) Evidence of crustal melting events
below the Island of Salina (Aeolian Arc, Southern Italy). Geol
Mag 141:525–540
Bull Volcanol (2013) 75:710 Page 11 of 11, 710
Geophys J Intern 162:633–640
Bansal AR, Gabriel G, Dimri VP, Krawczyk CM (2011) Estimation of
depth to the bottom of magnetic sources by a modified centroid
method for fractal distribution of sources: an application to
aeromagnetic data in Germany. Geophysics 76:L11–L22
Baranov V, Naudy H (1964) Numerical calculation of the formula of
reduction to the magnetic pole. Geophysics 29:67–79
Barberi F, Gandino A, Gioncada A, La Torre P, Sbrana A, Zenucchini
C (1994) The deep structure of the Eolian arc (Filicudi–Panarea–
Vulcano sector) in light of gravity, magnetic and volcanological
data. J Volcanol Geotherm Res 61:189–206
Blanco Montenegro I, De Ritis R, Chiappini M (2007) Imaging and
modelling the subsurface structure of volcanic calderas with highresolution
aeromagnetic data at Vulcano (Aeolian Islands, Italy).
Bull Volcanol 69(6):643–659. doi:10.1007/s00445-006-0100-7
Bouligand C, Glen JMG, Blakely RJ (2009) Mapping Curie temperature
depth in the western United States with a fractal model for
crustal magnetization. J Geophys Res 114:B11104. doi:10.1029/
2009JB006494
Boyce A (2007) Fluids in early stage hydrothermal alteration of highsulfidation
epithermal systems: a view from the Vulcano active
hydrothermal system (Aeolian Island, Italy). J Volcanol Geotherm
Res 166(2):76–90
Bruno PP, Paoletti V, Grimaldi M, Rapolla A (2000) Geophysical
exploration for geothermal low enthalpy resources in Lipari
Island, Italy. J Volcanol Geotherm Res 98:173–188
710, Page 10 of 11 Bull Volcanol (2013) 75:710
Chiappini M, Ferraccioli F, Bozzo E, Damaske D (2002) Regional
compilation and analysis of aeromagnetic anomalies for the
Transantarctic Mountains–Ross Sea sector of the Antarctic.
Tectonophysics 347:121–137
Castello B, Selvaggi G, Chiarabba C, Amato A (2005) Catalogo della
sismicità Italiana—CSI 10, 1981–2002, Cent Naz Terremoti, Ist
Naz di Geofis e. Vulcanol, Rome
Cicchino AMP, Zanella E, De Astis G, Lanza R, Lucchi F, Tranne CA,
Airoldi G, Mana S (2011) Rock magnetism and compositional
investigation of Brown Tuffs deposits at Lipari and Vulcano
(Aeolian Islands—Italy). J Volcanol Geotherm Res 208:23–38.
doi:10.1016/jjvolgeores201108007
De Astis G, Ventura G, Vilardo G (2003) Geodynamic significance of
the Aeolian volcanism (Southern Tyrrhenian Sea, Italy) in light of
structural, seismological and geochemical data. Tectonics
22:1040. doi:10.1029/2003TC001506
De Ritis R, Blanco-Montenegro I, Ventura G, Chiappini M (2005)
Aeromagnetic data provide new insights on the volcanism and
tectonics of Vulcano Island and offshore areas (southern
Tyrrhenian Sea, Italy). Geophys Res Lett 32:L15305. doi:10.1029/
2005GL023465
De Ritis R, Ventura G, Chiappini M (2007) Aeromagnetic anomalies
reveal hidden tectonic and volcanic structures in the central sector
of the Aeolian Islands, southern Tyrrhenian Sea, Italy. J Geophys
Res 112:B10. doi:10.1029/2006JB004639
De Rosa R, Guillou H, Mazzuoli R, Ventura G (2003a) New unspiked
K–Ar ages of volcanic rocks of the central and western sector of
the Aeolian Islands: reconstruction of the volcanic stages. J
Volcanol Geotherm Res 120:161–178
De Rosa R, Donato P, Gioncada A, Masetti M, Santacroce R (2003b)
The Monte Guardia eruption (Lipari, Aeolian Islands): an example
of reversely zoned magma mixing sequence. Bull Volcanol
65:530–543
Di Martino C, Frezzotti M, Lucchi F, Peccerillo A, Tranne C, Diamond
LW (2010) Magma storage and ascent at Lipari Island (Aeolian
Archipelago, Southern Italy) at 223–81 ka: the role of crustal
processes and tectonic influence. Bull Volcanol 72(9):1061–1076
Donato P, Behrens H, De Rosa R, Holtz F, Parat F (2006) Crystallization
conditions in Upper Pollara (Salina Island, Southern Tyrrhenian
Sea) magma chamber. Mineral Petrol 86:89–108
Faraone D, Silvano A, Verdiani G (1986) The monzogabbroic intrusion
in the island of Vulcano, Aeolian Archipelago, Italy. Bull
Volcanol 48:299–307
Fedi M, Quarta T, de Santis A (1997) Inherent power-law behavior of
magnetic field power spectra from a Spector and Grant ensemble.
Geophysics 62:1143–1150
Ferrucci F, Gaudiosi G, Milano G, Nercessian A, Vilardo G, Luongo G
(1991) Seismological exploration of Vulcano (Aeolian Islands,
Southern Tyrrhenian Sea): case history. Acta Vulcanol 1:143–152
Finn C, Sisson TW, Deszcz-Pan M (2001) Aerogeophysical measurements
of collapse–prone hydrothermally altered zones at Mount
Rainer volcano. Nature 409:600–603
Frezzotti ML, Peccerillo A, Bonelli R (2003) Magma ascent rates and
depths of magma reservoirs beneath the Aeolian volcanic arc
(Italy): inferences from fluid and melt inclusions in crustal xenoliths.
In: Bodnar B, De Vivo B (eds) Melt inclusions in volcanic
systems. Elsevier, Amsterdam, pp 185–206
Gambino S, Milluzzo V, Scaltrito A, Scarfì L (2012) Relocation and
focal mechanisms of earthquakes in the south-central sector of the
Aeolian Archipelago: new structural and volcanological insights.
Tectonophysics 524/525:108–115. doi:10.1016/jtecto201112024
Granieri D, Carapezza ML, Chiodini G (2006) Correlated increase in
CO2 fumarolic content and diffuse emission from La Fossa crater
(Vulcano, Italy): evidence of volcanic unrest or increasing gas
release from a stationary deep magma body? Geophys Res Lett
33:L13316. doi:10.1029/2006GL026460
Gvirtzman Z, Nur A (2001) Residual topography, lithospheric thickness,
and sunken slabs in the central Mediterranean. Earth Planet
Sci Lett 187:117–130
Lucchi F, Tranne CA, De Astis G, Keller J, Losito R, MorcheW(2008)
Stratigraphy and significance of Brown Tuffs of the Aeolian
Islands (southern Italy). J Volcanol Geotherm Res 117:49–70
Macmillan S, Maus D (2005) International geomagnetic reference
field—the tenth generation. Earth Planets Space 57:1135–1140
Maus S, Gordon D, Fairhead D (1997) Curie-temperature depth estimation
using a self-similar magnetization model. Geophys J
Intern 129:163–168. doi:10.1111/j1365-246X1997tb00945x
Maus S, Dimri VP (1996) Depth estimation from the scaling power
spectrum of potential fields? Geophys J Int 124:113–120
Mazzuoli R, Tortorici L, Ventura G (1995) Oblique rifting in Salina,
Lipari and Vulcano islands (Aeolian Islands, southern Italy). Terra
Nova 7:444–452
Nuccio PM, Paonita A (2001) Magmatic degassing of multicomponent
vapors and assessment of magma depth: application to Vulcano
Island (Italy). Earth Planet Sci Lett 193(3–4):467–481
Okubo Y, Graf RJ, Hansen RO, Ogawa K, Tsu H (1985) Curie-point
depths of the island of Kyushu and surrounding areas, Japan.
Geophysics 50:481–494
Pasquale V, Verdoya M, Chiozzi P (2003) Heat-flux budget in the
southeastern continental margin of the Tyrrhenian basin. Phys
Chem Earth 28:407–420
Peccerillo A, Frezzotti ML, De Astis G, Ventura G (2006) Modeling
the magma plumbing system of Vulcano (Aeolian Islands, Italy)
by integrated fluid-inclusion geobarometry, petrology, and
geophysics. Geology 34:17–20
Pilkington M, Todoeschuck JP (1993) Fractal magnetization of
continental crust. Geophys Res Lett 20:627–630
Ravat D, Salem A, Abdelaziz AMS, Elawadi E, Morgan P (2011)
Probing magnetic bottom and crustal temperature variations along
the Red Sea margin of Egypt. Tectonophysics 510:337–344
Ravat D, Pignatelli A, Nicolosi I, Chiappini M (2007) A study of spectral
methods of estimating the depth to the bottom of magnetic sources
from near-surface magnetic anomaly data. Geophys J Int 169:421–434
Romagnoli C, Calanchi N, Gabbianelli G, Lanzafame G, Rossi PL
(1989) Contributi delle ricerche di geologia marina alla
caratterizzazione morfostrutturale ed evolutiva dei complessi
vulcanici di Salina, Lipari e Vulcano (Isole Eolie). Boll Gruppo
Nazionale Vulcanologia 1989:971–978 (in italian)
Spector A, Grant FS (1970) Statistical models for interpreting
aeromagnetic data. Geophysics 35:293–302
Tanaka A, Okubo Y, Matsubayashi O (1999) Curie point depth based
on spectrum analysis of the magnetic anomaly data in East and
Southeast Asia. Tectonophysics 306:461–470
Tranne CA, Lucchi F, Calanchi N, Lanzafame G, Rossi PL (2002)
Geological map of the Island of Lipari (Aeolian Islands), scale
1:10000. University of Bologna and INGV, LAC Firenze
Ventura G, Vilardo G, Milano G, Pino NA (1999) Relationships among
crustal structure, volcanism and strike–slip tectonics in the Lipari–
Vulcano volcanic complex (Aeolian Islands, Southern Tyrrhenian
Sea, Italy). Phys Earth Planet Inter 116(1–4):31–52
Wang C, Hwang W, Shi Y (1989) Thermal evolution of a rift basin: the
Tyrrhenian Sea. J Geophys Res 94(B4):3991–4006
Zanella E, Lanza R (1994) Remanent and induced magnetization in the
volcanites of Lipari and Vulcano (Aeolian Islands). Annals
Geophys 37:1149–1156
Zanon V, Frezzotti ML, Peccerillo A (2003) Magmatic feeding system
and crustal magma accumulation beneath Vulcano Island (Italy):
evidence from CO2 fluid inclusions in quartz xenoliths. J
Geophys Res 108:2298–2301. doi:10.1029/2002JB002140
Zanon V, Nikogosian IK (2004) Evidence of crustal melting events
below the Island of Salina (Aeolian Arc, Southern Italy). Geol
Mag 141:525–540
Bull Volcanol (2013) 75:710 Page 11 of 11, 710
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