Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/4643
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dc.contributor.authorallCivile, D.; Istituto Nazionale di Oceanografia e Geofisica Sperimentale (OGS), Trieste, Italyen
dc.contributor.authorallLodolo, E.; Istituto Nazionale di Oceanografia e Geofisica Sperimentale (OGS), Trieste, Italyen
dc.contributor.authorallTortorici, L.; Dipartimento di Scienze Geologiche, Università di Catania, Catania, Italyen
dc.contributor.authorallLanzafame, G.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Catania, Catania, Italiaen
dc.contributor.authorallBrancolini, G.; Istituto Nazionale di Oceanografia e Geofisica Sperimentale (OGS), Trieste, Italyen
dc.date.accessioned2008-12-12T08:58:09Zen
dc.date.available2008-12-12T08:58:09Zen
dc.date.issued2008en
dc.identifier.urihttp://hdl.handle.net/2122/4643en
dc.description.abstractField geological data of the Pantelleria Island, a large Late Quaternary volcano located in the Sicily Channel rift zone, integrated with offshore geophysical information, are used to derive the structural setting of the Island and the surrounding region, and to analyse the relationships between tectonics and magmatism. Field work shows that the principal faults exposed on the Island fall into two systems trending NNE–SSW and NW–SE. Mapped faults from offshore multichannel seismic profiles show similar trends, and some of them represent the offshore extension of the Pantelleria Island structures. The NW–SE faults bound the Pantelleria Graben, one of the three main depressions formed since the Late Miocene–Early Pliocene within the African continental platform, which compose the Sicily Channel rift zone. A 3-D Moho depth geometry, derived from inversion of Bouguer gravity data, shows a significant uplift of the discontinuity up to 16–17 km beneath the westernmost part of the Pantelleria Graben and beneath the Pantelleria Island; it lows rapidly to 24–25 km away from the graben northeastward and south-westward. The Moho uplift could explain the presence of a shallow magma chamber in the southern part of the Island, where processes of magmatic differentiation are documented. Geological and geophysical data suggest that the northwestern part of the Sicily Channel is presently dominated by a roughly E–W directed extensional regime. Crustal cracking feeding the Quaternary volcanism could be also related to this extensional field that would be further responsible for the development of the N–S trending volcanic belt that extends in the Sicily Channel from Lampedusa Island to the Graham Bank. This mode of deformation is confirmed also by geodetic data. This implies that in the northwestern part of the Sicily Channel, the E–W extension replaced the NE–SW crustal stretching that originated the NW-trending tectonic depressions constituting the rift zone. © 2008 Elsevier B.V. All rights reserved.en
dc.language.isoEnglishen
dc.publisher.nameElsevieren
dc.relation.ispartofMarine Geologyen
dc.relation.ispartofseries1-2/251(2008)en
dc.subjectPantelleria Islanden
dc.subjectChannel rift zoneen
dc.subjectstructural analysisen
dc.subjectQuaternary volcanismen
dc.subjectgravity modellingen
dc.subjecttectonic extensionen
dc.titleRelationships between magmatism and tectonics in a continental rift: The Pantelleria Island region (Sicily Channel, Italy)en
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber32-46en
dc.subject.INGV04. Solid Earth::04.04. Geology::04.04.09. Structural geologyen
dc.identifier.doi10.1016/j.margeo.2008.01.009en
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Petrol. 1979 pp. 377-388 Cello, G., "Structure and deformation processes in the Strait of Sicily “rift zone”" Tectonophysics 1987 pp. 237-247 Cello, G.; Crisci, M.; Marabini, S.; Tortorici, L., "Transtensive tectonics in the Strait of Sicily: structural and volcanological evidence from the Island of Pantelleria" Tectonics 1985 pp. 311-322 Chierici, R.; Grassi, S.; La Rosa, N.; Nannini, R.; Squarci, P.; Zurlo, R., Proc. World Geothermal Congress, Florence (Italy), May 18-31, (1995) Civetta, L.; Cornette, Y.; Crisci, G.; Gillot, P.-Y.; Orsi, G.; Requejos, C.S., "Geology, geochronology and chemical evolution of the Island of Pantelleria" Geol. Mag. 1984 pp. 541-668 Civetta, L.; Cornette, Y.; Gillot, P.-Y.; Orsi, G., "The eruptive history of Pantelleria (Sicily Channel) in the last 50 ka" Bull. 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Res. 2004 pp. B11402 Della Vedova, B.; Pellis, G.; Corubolo, P., Atti 6° Convegno GNGTS, CNR Roma, (1987) Finetti, I.R., "Geophysical study of the Sicily Channel rift zone" Boll. Geofis. Teor. Appl. 1984 pp. 3-28 Finetti, I.R.; Del Ben, A., Finetti, I.R., Editor, CROP PROJECT: Deep Seismic Exploration of the Central Mediterranean and Italy, Elsevier B.V., (2005) Hollenstein, C.H.; Kahle, H.G.; Geiger, A.; Jenny, S.; Goes, S.; Giardini, D., "New GPS constraints on the Africa–Eurasia plate boundary zone in southern Italy" Geophys. Res. Lett. 2003 pp. 1935 Illies, J.H., "Graben formation – the Maltese Islands – a case history" Tectonophysics 1981 pp. 151-168 Jongsma, D.; Van Hinte, J.E.; Woodside, J.M., "Geologic structure and neotectonics of the North African continental margin south of Sicily" Mar. Pet. Geol. 1985 pp. 156-179 Lanzafame, G., Rossi, P.L., Tranne, C.A., Lanti, E., 1994. Carta geologica dell'Isola di Linosa 1:5000. Selca, Firenze, Italy. Mahood, G.A.; Hildreth, W., "Geology of the peralkaline volcano at Pantelleria, Strait of Sicily" Bull. Volcanol. 1986 pp. 143-172 Maldonado, A.; Stanley, D.I., "Lithofacies as a function of depth in the Strait of Sicily" Geology 1977 pp. 111-117 Morelli, C.; Gantar, C.; Pisani, M., "Bathymetry, gravity and magnetism in the Straits of Sicily and Ionian Sea" Boll. Geofis. Teor. Appl. 1975 pp. 39-58 Pe-Piper, G.; Piper, D.J.W.; Perissoratis, C., "Neotectonics and the Kos Plateau Tuff eruption of 161 ka, South Aegean arc" J. Volcanol. Geotherm. Res. 2005 pp. 315-338 Bibliographic Page Full Text Reuther, C.D.; Eisbacher, G.H., "Pantelleria rift-crustal extension in a convergent intraplate setting" Geol. Rundsch. 1985 pp. 585-597 Riccò, A., "Terremoti, sollevamento ed eruzione sottomarina a Pantelleria nella seconda metà dell'ottobre 1891" Boll. Soc. Geogr. Ital. 1892 pp. 1-31 Rossi, P.L.; Tranne, C.A.; Calanchi, N.; Lanti, E., "Geology, stratigraphy and volcanology evolution of the Island of Linosa (Sicily Channel)" Acta Vulcanol. 1996 pp. 73-90 Rotolo, S.G.; Castorina, F.; Cellula, D.; Pompilio, M., "Petrology and Geochemistry of Submarine Volcanism in the Sicily Channel" J. Geol. 2006 pp. 355-365 Scarascia, S.; Cassinis, R.; Lozej, A.; Nebuloni, A., "A seismic and gravimetric model of crustal structures across the Sicily Channel Rift Zone" Boll. Soc. Geol. Ital. 2000 pp. 213-222 Squarci, P.; Gianelli, S.; Grassi, S.; Mussi, M.; D'Amore, F., "Preliminary results of geothermal prospecting on the Island of Pantelleria (Italy)" Acta Vulcanol. 1994 pp. 117-123 Torelli, L.; Zitellini, N.; Argnani, A.; Brancolini, G.; De Cillia, C.; Peis, D.; Tricart, P., "Sezione geologica crostale dall'avampaese Pelagiano al Bacino di retroarco Tirrenico (Mediterraneo centrale)" Mem. Soc. Geol. Ital. 1991 pp. 385-399 Washington, H.S., "The submarine eruption of 1831 and 1891 near Pantelleria" Am. J. Sci. 1909 pp. 131-150 Winnock, E., Wezel, I.F.C., Editor, Sedimentary Basins of Mediterranean Margins, Tecnoprint, Bologna, (1981) Zolotarev, V.G.; Sochelnikov, V.V., "Geothermal conditions of the African–Sicilian rise" Izv. - Acad. Sci. USSR, Phys. Solid Earth 1980 pp. 202-206en
dc.description.obiettivoSpecifico3.2. Tettonica attivaen
dc.description.journalTypeJCR Journalen
dc.description.fulltextreserveden
dc.contributor.authorCivile, D.en
dc.contributor.authorLodolo, E.en
dc.contributor.authorTortorici, L.en
dc.contributor.authorLanzafame, G.en
dc.contributor.authorBrancolini, G.en
dc.contributor.departmentIstituto Nazionale di Oceanografia e Geofisica Sperimentale (OGS), Trieste, Italyen
dc.contributor.departmentIstituto Nazionale di Oceanografia e Geofisica Sperimentale (OGS), Trieste, Italyen
dc.contributor.departmentDipartimento di Scienze Geologiche, Università di Catania, Catania, Italyen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italiaen
dc.contributor.departmentIstituto Nazionale di Oceanografia e Geofisica Sperimentale (OGS), Trieste, Italyen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextrestricted-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptIstituto Nazionale Di Oceanografia E Di Geofisica Sperimentale - OGS-
crisitem.author.deptOsservatorio Geofisico Sperimentale, Trieste, Italia-
crisitem.author.deptDipartimento di Scienze Geologiche, Università di Catania, Catania, Italy-
crisitem.author.deptOsservatorio Geofisico Sperimentale, Trieste, Italy-
crisitem.author.orcid0000-0002-2809-0015-
crisitem.author.orcid0000-0002-4706-2095-
crisitem.classification.parent04. Solid Earth-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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