Please use this identifier to cite or link to this item:
http://hdl.handle.net/2122/5650
DC Field | Value | Language |
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dc.contributor.authorall | Nigro, F.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italia | en |
dc.contributor.authorall | Salvaggio, G.; Dipartimento di Geologia e Geodesia, Università di Palermo, Italy - Via Archirafi, 22, 90123, Palermo | en |
dc.contributor.authorall | Favara, R.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italia | en |
dc.contributor.authorall | Renda, P.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italia | en |
dc.date.accessioned | 2010-01-18T12:17:44Z | en |
dc.date.available | 2010-01-18T12:17:44Z | en |
dc.date.issued | 2009 | en |
dc.identifier.uri | http://hdl.handle.net/2122/5650 | en |
dc.description.abstract | Sicily owes its complex geological structure to a switch in tectonic regime from the Mesozoic to the Tertiary. A set of tectonic units outcrops in the northern portion of the island that originated during the Tertiary at the expense of paleogeographic domains of the African Mesozoic continental margin. The pre-orogenic successions show different types of deformation (extensional and transcurrent) related to the Jurassic paleotectonic evolution of the southern Neotethys margin. The history of the tectonic inversion of the Neotethys shear zone is recorded in the Cretaceous strata. Extension occurred during late Cretaceous and may be compatible with the tensile stress field related to the Sicilide basin opening. The Neogene deformations are linked to collisional processes and are mostly represented by thrusts and folds. Since the late Miocene onwards, the formation of the Tyrrhenian basin has driven the recent tectonic evolution of Northern Sicily. Its basin formation was realised through extension, followed by transcurrent tectonics along its southern margin. | en |
dc.language.iso | English | en |
dc.publisher.name | Società Geologica Italiana | en |
dc.relation.ispartof | Rendiconti online Società Geologica Italiana | en |
dc.relation.ispartofseries | /5(2009) | en |
dc.subject | cronologia delle deformazioni mesozoico-terziarie | en |
dc.subject | Sicilia centro-settentrionale | en |
dc.title | Evoluzione tettonica mesozoico-terziaria della Sicilia centrosettentrionale | en |
dc.type | article | en |
dc.description.status | Published | en |
dc.type.QualityControl | Peer-reviewed | en |
dc.description.pagenumber | 148-152 | en |
dc.subject.INGV | 04. Solid Earth::04.04. Geology::04.04.09. Structural geology | en |
dc.subject.INGV | 04. Solid Earth::04.07. Tectonophysics::04.07.07. Tectonics | en |
dc.relation.references | CATALANO R. & D'ARGENIO B. (1982) - Schema geologico della Sicilia. In: Catalano R. & D'Argenio B. (Eds.), "Guida alla Geologia della Sicilia Occidentale”, Guide Geologiche Regionali, Mem. Soc. Geol. It., Suppl. A., 24, 9-41. GIUNTA G., NIGRO F. & RENDA P. (2000a) - Extensional Tectonics during Maghrebides Chain Building since Late Miocene: examples from Northern Sicily. A.S.G.P., 70, 1- 18. GIUNTA G., NIGRO F., RENDA P. & GIORGIANNI A. (2000b) - The Sicilian-Maghrebides Tyrrhenian Margin: a neotectonic evolutionary model. Boll. Soc. Geol. It., 119, 553-565. GIUNTA G., NIGRO F. & RENDA P. (2003) - The Mesozoic continental break-up geometry of the Sicilian Tunisian Meghrebides: an updated model. In: Salem M. J., Oun K. M. & Seddiq H. M. (eds), “The Geology of Northwest Libya”, Sedimentary basins of Libya, III, 156-169. NIGRO F. & RENDA P. (1999) – Evoluzione geologica ed assetto strutturale della Sicilia centro-settentrionale. Boll. Soc. Geol. It., 118, 375-388. NIGRO F. & RENDA P. (2000) - Un modello di evoluzione tettono-sedimentaria dell’avanfossa neogenica siciliana. Boll. Soc. Geol. It., 219, 667-686. NIGRO F. & RENDA P. (2001) - Late Miocene-Quaternary stratigraphic record in the Sicilian Belt (Central Mediterranean): tectonics versus eustasy. Boll. Soc. Geol. It., 120, 151-164. NIGRO F. E RENDA P. (2002) - From Mesozoic extension to Tertiary collision: deformation pattern in the northern Sicily chain units. Boll. Soc. Geol. It., 121, 87-97. NIGRO F. & RENDA P. (2004) - The contribution of the preexisting structures in mountain belt evolution: the example of the negative inversion in Northern Sicily. Boll. Soc. Geol. It., 123, 175-187. NIGRO F. & RENDA P. (2005) - transtensional/extensional fault activity from the Mesozoic rifting to Tertiary chain building in Northern Sicily (Central Mediterranean). Geol. Carpathica., 56, 255-271. NIGRO F., SALVAGGIO G., RENDA P. & FAVARA R. (20008) - Extensional deformations during Neogene chain building in Sicily. Boll. Soc. Geol. It., in stampa. RENDA P., TAVARNELLI E., TRAMUTOLI M. & GUEGUEN E. (2000) - Neogene deformations in the central Madonie Mountains (northern Sicily, Italy) and their significance in the geodynamic evolution of the southern Tyrrhenian Sea margin. Mem. Soc. Geol. It., 55, 38-47. SCANDONE P., GIUNTA G. & LIGUORI V. (1974) - The connection between Apulia and Sahara continental margins in the Southern Apennines and in Sicily. Mem. Soc. Geol. It., 13, 317-323. | en |
dc.description.obiettivoSpecifico | 3.3. Geodinamica e struttura dell'interno della Terra | en |
dc.description.journalType | N/A or not JCR | en |
dc.description.fulltext | reserved | en |
dc.contributor.author | Nigro, F. | en |
dc.contributor.author | Salvaggio, G. | en |
dc.contributor.author | Favara, R. | en |
dc.contributor.author | Renda, P. | en |
dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italia | en |
dc.contributor.department | Dipartimento di Geologia e Geodesia, Università di Palermo, Italy - Via Archirafi, 22, 90123, Palermo | en |
dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italia | en |
dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italia | 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 | Dipartimento di Geologia e Geodesia, Università di Palermo, Italy - Via Archirafi, 22, 90123, Palermo | - |
crisitem.author.dept | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Palermo, Palermo, Italia | - |
crisitem.author.dept | Universita' di Palermo | - |
crisitem.author.orcid | 0000-0003-4588-2935 | - |
crisitem.author.orcid | 0000-0002-4921-4427 | - |
crisitem.author.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
crisitem.author.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
crisitem.classification.parent | 04. Solid Earth | - |
crisitem.classification.parent | 04. Solid Earth | - |
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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Nigro et al_GIGS 2009_B.pdf | Main article | 830.21 kB | Adobe PDF |
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