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The 8.2-event record on the Alicante marine continental shelf (SE, Spain)

dc.contributor.authorTent Manclús, José Enrique
dc.contributor.authorEstévez, Antonio
dc.contributor.authorSoria, Jesús M.
dc.contributor.authorBenabdeloued, Nassim Y.B.
dc.contributor.authorCorbí, Hugo
dc.contributor.authorRey Salgado, Jorge
dc.contributor.authorPina, José Antonio
dc.contributor.authorYébenes, Alfonso
dc.description.abstractHigh resolution seismic profiles of the Alicante continental shelf have been studied identifying a seismic prism which top at about -20 m below today sea-level. The prism is covered by recent sediments and can be interpreted as formed during a short interval of stand-by in the general transgression after the last glacial maximum. The -20 m level have been compared with the holocene Mediterranean sea-level-curve to propose an age of about 8 ka BP coinciding with the «8.2 ka cooling event» that was an abrupt, widespread climate instability. The prism top is deeper in the northern seismic profiles thus indicating a more subsidence that the southern coastal shelf where an erosion surface with rocky shoals configure the sea bottomen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España
dc.subject.otherAlicante continental shelfen_US
dc.subject.other8.2 ka eventen_US
dc.subject.otherHigh-resolution seismicen_US
dc.subject.otherSea-level changesen_US
dc.titleRegistro del evento 8.2 ka en la plataforma continental de Alicante (SE, España)en_US
dc.titleThe 8.2-event record on the Alicante marine continental shelf (SE, Spain)eng

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