Evidence of tectonic control on active arc volcanism: The Panarea-Stromboli tectonic link inferred by submarine hydrothermal vents monitoring (Aeolian arc, Italy)

Geophysical Research Letters

Volumn 36, Issue 4, 2009, Pages

  Heinicke, J ^a   Italiano, F ^b   Maugeri, R ^b   Merkel, B ^a   Pohl, T ^c   Schipek, M ^a   Braun, T ^d  

^a TU BERGAKADEMIE FREIBERG   (Germany)

^b SEZIONE DI PALERMO   (Italy)

^c Geo Dive   (Germany)

^d ISTITUTO NAZIONALE DI GEOFISICA E VULCANOLOGIA   (Italy)

Author keywords

[No Author keywords available]

Indexed keywords

3HE/4HE RATIO; ACTIVE TECTONICS; AEOLIAN ISLANDS , ITALY; ARC VOLCANISM; CONTINUOUS MONITORING; GEOCHEMICAL METHODS; HYDROTHERMAL SYSTEM; HYDROTHERMAL VENT; MAGMATIC FLUIDS; PANAREA; SEISMIC ACTIVITY; STROMBOLI VOLCANO; TECTONIC ACTIVITY; TECTONIC CONTROL; VOLCANIC ARC; VOLCANIC COMPLEX; VOLCANIC EDIFICE; VOLCANIC RISK; VOLCANIC UNREST;

CAVITY RESONATORS; GROUNDWATER FLOW; HOT SPRINGS; METEOROLOGICAL INSTRUMENTS; SUBMARINES; TECTONICS;

VOLCANOES;

CRATER; FLUID FLOW; HYDROTHERMAL SYSTEM; HYDROTHERMAL VENT; SEISMICITY; VOLCANISM;

EURASIA; EUROPE; ITALY; LIPARI ISLANDS; MESSINA [SICILY]; PANAREA; SICILY; SOUTHERN EUROPE; STROMBOLI;

EID: 66149166162     PISSN: 00948276     EISSN: None     Source Type: Journal    
DOI: 10.1029/2008GL036664     Document Type: Article

References (21)

1. Aliani, S., R. Meloni, and P. K. Dando (2004), Periodicities in sediment temperature time-series at a marine shallow water hydrothermal vent in Milos Island (Aegean Volcanic arc, eastern Mediterranean), J. Mar. Syst., 46, 109-119.
2. Azzaro, R., M. S. Barbano, R. Camassi, S. D'Amico, A. Mostaccio, G. Piangiamore, and L. Scarfi (2004), The earthquake of 6 September 2002 and the seismic history of Palermo (northern Sicily, Italy): Implications for the seismic hazard assessment of the city, J. Seismol., 8, 525-543.
3. Calanchi, N., A. Peccerillo, C. A. Tranne, F. Lucchini, P. L. Rossi, P. Kempton, M. Barbieri, and T. W. Wu (2002), Petrology and geochemistry of volcanic rocks from the island of Panarea: Implications for mantle evolution beneath the Aeolian island arc (southern Tyrrhenian Sea), J. Volcanol. Geotherm. Res., 115, 367-395.
4. Caliro, S., A. Caracausi, G. Chiodini, M. Ditta, F. Italiano, M. Longo, C. Minopoli, P. M. Nuccio, A. Paonita, and A. Rizzo (2004), Evidence of a recent input of magmatic gases into the quiescent volcanic edifice of Panarea, Aeolian Islands, Italy, Geophys. Res. Lett., 31, L07619, doi:10.1029/ 2003GL019359.
5. Capaccioni, B., F. Tassi, O. Vaselli, D. Tedesco, and R. Poreda (2007), Submarine gas burst at Panarea Island (southern Italy) on 3 November 2002: A magmatic versus hydrothermal episode, J. Geophys. Res., 112, B05201, doi:10.1029/2006JB004359.
6. Caracausi, A., M. Ditta, F. Italiano, M. Longo, P. M. Nuccio, A. Paonita, and A. Rizzo (2005a), Changes in fluid geochemistry and physico-chemical conditions of geothermal systems caused by magmatic input: The recent abrupt outgassing off the island of Panarea (Aeolian Islands, Italy), Geochim. Cosmochim. Acta, 69, 3045-3059.
7. Caracausi, A., M. Ditta, F. Italiano, M. Longo, P. M. Nuccio, and A. Paonita (2005b), Massive submarine gas output during the volcanic unrest off Panarea Island (Aeolian arc, Italy): Inferences for explosive conditions, Geochem. J., 39, 459-467.
8. Cesca, S., T. Braun, E. Tessmer, and T. Dahm (2007), Modelling of the April 5, 2003, Stromboli (Italy) paroxysmal eruption from the inversion of broadband seismic data, Earth Planet Sci. Lett., 261, 164-178.
9. Chen, C.-T. A., Z. Zeng, F.-W. Kuo, T. F. Yang, B.-J. Wang, and Y.-Y. Tu (2005), Tide-influenced acidic hydrothermal system offshore NE Taiwan, Chem. Geol, 224, 69-81.
10. Chouet, B., P. Dawson, T. Ohminato, M. Martini, G. Saccorotti, F. Giudi-cepietro, G. De Luca, G. Milana, and R. Scarpa (2003), Source mechanisms of explosions at Stromboli volcano, Italy, determined from moment-tensor inversions of very-long-period data, J. Geophys. Res., 70S(B1), 2019, doi:10.1029/2002JB001919.
11. Dahm, T, M. Thorwart, E. R. Flueh, T Braun, R. Herber, P. Favali, L. Beranzoli, G. D'Anna, F. Frugoni, and G. Smriglio (2002), Ocean bottom seismometers deployed in Tyrrhenian Sea, Eos Trans. AGU, 83, 309.
12. Esposito, A., G. Giordano, and M. Anzidei (2006), The 2002-2003 submarine gas eruption at Panarea volcano (Aeolian Islands, Italy): Volca-nology of the seafloor and implications for the hazard scenario, Mar. Geol., 227, 119-134.
13. Gamberi, F., P. M. Marani, and C. Savelli (1997), Tectonic volcanic and hydrothermal features of submarine portion of Aeolian arc (Tyrrhenian Sea), Mot Geol, 140, 167-181.
14. Italiano, F and P. M. Nuccio (1991), Geochemical investigations of submarine volcanic exhalations to the east of Panarea, Aeolian Islands, Italy, J. Volcanol. Geotherm. Res., 46, 125-141.
15. James, M. R., S. J. Lane, B. Chouet, and J. S. Gilbert (2004), Pressure changes associated with the ascent and bursting of gas slugs in liquid-filled vertical and inclined conduits, J. Volcanol. Geotherm. Res., 129, 61-82.
16. Leighton, T G. (1994), The Acoustic Bubble, Academic, London.
17. Martelli, M., P. M. Nuccio, F. M. Stuart, V. Di Liberto, and R. M. Ellam (2008), Constraints on mantle source and interactions from He-Sr isotope variation in Italian Plio-Quatemary volcanism, Geochem. Geophys. Geo-syst., 9, Q02001, doi:10.1029/2007GC001730.
18. Mercalli, G. (1883), Vulcani e Fenomeni Vulcanici, Geol. Hal, vol. 3, edited by G. Negri, A. Stoppani, and G. Mercalli, 374 pp., F. Vallardi, Milan, Italy.
19. Patané, D., M. Mattia, G. Di Grazia, F. Cannavó, E. Giampiccolo, C. Musumeci, P. Montalto, and E. Boschi (2007), Insights into the dynamic processes of the 2007 Stromboli eruption and possible meteorological influences on the magmatic system, Geophys. Res. Lett., 34, L22309, doi: 10.1029/2007GL031730.
20. Ripepe, M., E. Marchetti, P. Poggi, A. Harris, A. Fiaschiand, and G. Ulivieri (2004), Seismic, acoustic, and thermal network monitors the 2003 eruption of Stromboli Volcano, Eos Trans. AGU, 85, -329-332.
21. Sohn, R. A. (2007), Stochastic analysis of exit fluid temperature records from the active TAG hydrothermal mound (Mid-Atlantic Ridge, 26°N): 1. Modes of variability and implications for subsurface flow, J. Geophys. Res., 112, B07101, doi:10.1029/2006JB004435.