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http://hdl.handle.net/10261/27364
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Campo DC | Valor | Lengua/Idioma |
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dc.contributor.author | Ercilla, Gemma | - |
dc.contributor.author | Córdoba, Diego | - |
dc.contributor.author | Gallart Muset, Josep | - |
dc.contributor.author | Gràcia, Eulàlia | - |
dc.contributor.author | Muñoz, Josep A. | - |
dc.contributor.author | Somoza, Luis | - |
dc.contributor.author | Vázquez, Juan Tomás | - |
dc.contributor.author | PRESTIGE Group | - |
dc.date.accessioned | 2010-09-01T08:41:42Z | - |
dc.date.available | 2010-09-01T08:41:42Z | - |
dc.date.issued | 2006 | - |
dc.identifier.citation | Marine Pollution Bulletin 53(5-7): 208-219 (2006) | en_US |
dc.identifier.issn | 0025-326X | - |
dc.identifier.uri | http://hdl.handle.net/10261/27364 | - |
dc.description | Special issue The Prestige Oil Spill: A Scientific Response.-- 12 pages, 11 figures | en_US |
dc.description.abstract | The tanker Prestige sank off NW Iberia on the 19th November 2002. The stern and bow of the Prestige wreck are located on the southwestern edge of the Galicia Bank, at 3565 m and 3830 m water depths, respectively. This bank is a structural high controlled by major faults with predominant N–S, NNE–SSW, and NNW–SEE trends. It is characterized by moderate to low seismic activity. The faults have controlled the local depositional architecture, deforming, fracturing, relocating and distributing sediments since the Valangian (early Cretaceous). The Prestige sinking area corresponds to an asymmetric half-graben structure with a N–S trend, which conditions the present-day morphology. The faulted flank outcrops and its activity and erosion have favoured the occurrence of mass-movements (slumps, slump debris, mass-flows and turbidity currents), building valleys and depositional lobes. Nearsurface sediments comprise mostly terrigenous and biogenous turbiditic muds and sands with a minor presence of hemipelagic muds, except on the fault scarp where pelagites predominate. Potential geological hazards resulting from tectonic and sedimentary processes affect almost the entire Prestige sinking area | en_US |
dc.description.sponsorship | This research was supported by the Project “Identificación de Riesgos Geoambientales y su Valoración en la Zona de Hundimiento del Buque Prestige” from the Science and Technology Ministry | en_US |
dc.format.extent | 5867 bytes | - |
dc.format.mimetype | application/pdf | - |
dc.language.iso | eng | en_US |
dc.publisher | Elsevier | en_US |
dc.rights | closedAccess | en_US |
dc.subject | Prestige | en_US |
dc.subject | Galicia Bank | en_US |
dc.subject | Morphology | en_US |
dc.subject | Sedimentology | en_US |
dc.subject | Geological hazards | en_US |
dc.title | Geological characterization of the Prestige sinking area | en_US |
dc.type | artículo | en_US |
dc.identifier.doi | 10.1016/j.marpolbul.2006.03.016 | - |
dc.description.peerreviewed | Peer reviewed | en_US |
dc.relation.publisherversion | https://doi.org/10.1016/j.marpolbul.2006.03.016 | en_US |
dc.type.coar | http://purl.org/coar/resource_type/c_6501 | es_ES |
item.cerifentitytype | Publications | - |
item.openairecristype | http://purl.org/coar/resource_type/c_18cf | - |
item.grantfulltext | none | - |
item.openairetype | artículo | - |
item.fulltext | No Fulltext | - |
item.languageiso639-1 | en | - |
Aparece en las colecciones: | (ICM) Artículos (UTM) Artículos (Geo3Bcn) Artículos (IGME) Artículos |
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