Please use this identifier to cite or link to this item:
http://hdl.handle.net/2122/8261
DC Field | Value | Language |
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dc.contributor.authorall | Italiano, F.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italia | en |
dc.contributor.authorall | Maugeri, R.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Catania, Catania, Italia | en |
dc.contributor.authorall | Mastrolia, A.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italia | en |
dc.contributor.authorall | Jens, H.; Sächsische Akademie der Wissenschaften zu Leipzig, TU Freiberg, Germany | en |
dc.date.accessioned | 2012-10-18T07:21:25Z | en |
dc.date.available | 2012-10-18T07:21:25Z | en |
dc.date.issued | 2011 | en |
dc.identifier.uri | http://hdl.handle.net/2122/8261 | en |
dc.description.abstract | The hydrothermal activity represents an evidence of high-energy submarine processes related to active or recent volcanism. Shallow hydrothermal vents represent a unique study opportunity due to the easy access to the vented fluids. The hydrothermal fluids released off the coast of Panarea Island (Aeolian arc, Italy) have been intensively investigated since mid 80’s. The sudden unrest of submarine volcanic activity occurred on November 2002 with a submarine low-energy explosion, dramatically changed the geochemical features and the degassing rate of the submarine hydrothermal vents and pushed the scientists to develop new methods to monitor the venting activity. A better inside of the whole submarine hydrothermal system has been achieved by the development of new investigations methods and geochemical models. The new information closely linking the geothermal and the volcanic activity of the Island require that a continuous monitoring of the submarine hydrothermal activity is carried out. A new sea-floor observatory has been developed for multidisciplinary monitoring activity and to perform real-time data transmission from the sea bottom. Among the other sensors, an acoustic probe, installed for a long-term recording of the sound of the bubbling gases in a frequency range of 0.5-3 kHz, gave useful information of a tight link between the submarine volcanic activity of Panarea Island and the crater explosions of the nearby active volcanic island of Stromboli | en |
dc.language.iso | English | en |
dc.publisher.name | Elsevier | en |
dc.relation.ispartof | Procedia Earth and Planetary Science | en |
dc.relation.ispartofseries | /4 (2011) | en |
dc.subject | Seafloor observatory | en |
dc.subject | hydrothermal vents | en |
dc.title | SMM, a new seafloor monitoring module for real-time data transmission: an application to shallow hydrothermal vents | en |
dc.type | article | en |
dc.description.status | Published | en |
dc.type.QualityControl | Peer-reviewed | en |
dc.description.pagenumber | 93-98 | en |
dc.subject.INGV | 03. Hydrosphere::03.01. General::03.01.08. Instruments and techniques | en |
dc.identifier.doi | 10.1016/j.proeps.2011.11.010 | en |
dc.relation.references | Lupton J, C de Ronde, M Sprovieri, E.T. Baker, P. P Bruno, F. Italiano, S. Walker, K. Faure), M. Leybourne, K. Britten, R. Greene (2010) Active Hydrothermal Discharge on the Submarine Aeolian Arc: New Evidence from Water Column Observations. Jour. Geophys. Res., 116, B02102, doi:10.1029/2010JB007738 [2] Maugeri T.L., Bianconi G., Canganella F., Danovaro R., Gugliandolo C., Italiano F., Lentini V., Manini E., Nicolaus B. (2009) Shallow hydrothermal vents in the southern Tyrrhenian Sea. Chem and Ecology, 26, 1, 1-14 [3] F. Italiano (2009) Hydrothermal fluids vented at shallow depths at the Aeolian islands: relationships with volcanic and geothermal systems. Proceedings International Workshop on Research In Shallow Marine And Fresh Water Systems, 39, 55-60. Freiberg, Germany, 14-16 May, 2009. [4] Caracausi A., Ditta M., Italiano F., Longo M., Nuccio P.M., Paonita A. (2005) Massive submarine gas output during the volcanic unrest off Panarea Island (Aeolian arc, Italy): inferences for explosive conditions. Geochemical Journal, 39, 5, 449-467 [5] Aliani, S., Meloni, R. and Dando, P.R. (2004), Periodicities in sediment temperature time-series at a marine shallow water hydrothermal vent in Milos Island (Aegean Volcanic arc, Eastern Mediterranean). J. Mar. Systems, 46 (1-4), 109-119 [6] Chen T.A.C, Zeng Z, Kuo F, Yang T F, Wang B.J., Tu Y. (2005). Tide-influenced acidic hydrothermal system offshore NE Taiwan. Chem. Geol., 224 (1-3), 69-81. [7] Sohn, R.A., 2007. Stochastic analysis of exit fluid temperature records from active TAG hydrothermal mound (Mid- Atlantic Ridge, 26 degrees N): 1. Modes of variability and implications for the subsurface flow. J. Geophys. Res., 112 B07101, doi:10.1029/2006JB004435 [8] Leighton T.G., (1994). The acoustic bubble, Academic Press, London [9] Heinicke J., Italiano F., Maugeri R., Merkel B., Pohl T., Schipeck M. (2009) Evidence of tectonic control on active arc volcanism: The Panarea-Stromboli tectonic link inferred by submarine hydrothermal vents monitoring (Aeolian arc, Italy), Geophys. Res. Lett., 36, L04301, doi:10.1029/2008GL036664 | en |
dc.description.obiettivoSpecifico | 1.8. Osservazioni di geofisica ambientale | en |
dc.description.journalType | N/A or not JCR | en |
dc.description.fulltext | restricted | en |
dc.relation.eissn | 1878-5220 | en |
dc.contributor.author | Italiano, F. | en |
dc.contributor.author | Maugeri, R. | en |
dc.contributor.author | Mastrolia, A. | en |
dc.contributor.author | Jens, H. | en |
dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, 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 Palermo, Palermo, Italia | en |
dc.contributor.department | Sächsische Akademie der Wissenschaften zu Leipzig, TU Freiberg, Germany | 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 Palermo, Palermo, 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 Palermo, Palermo, Italia | - |
crisitem.author.dept | Sächsische Akademie der Wissenschaften zu Leipzig, TU Freiberg, Germany | - |
crisitem.author.orcid | 0000-0002-9465-6398 | - |
crisitem.author.orcid | 0000-0003-4330-3434 | - |
crisitem.author.orcid | 0000-0001-6082-208X | - |
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 | 03. Hydrosphere | - |
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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