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Sedimentary structuration ofHolocene deltaic bodies in northem Alboran Sea margin

dc.contributor.authorHernández Molina, F. Javier
dc.contributor.authorVázquez Garrido, Juan Tomás
dc.contributor.authorSomoza, L.
dc.contributor.authorRey Salgado, Jorge
dc.description.abstractIn three deltaic areas of northem Alboran Sea margin, the different depositional bodies that establish the sedimentary structure of the holocene progradational wedge has been determinated by high resolution seismic profile (3.5 kHz). Four seismic units have been diferenciated: FI seismic unit (a weak one with an oblicuo-progradational reflection configuration), F2 seismic unit (transparent), F3 seismic unit (a weak one with a sigmoidal-oblique reflection configuration), and F4 seismic unit (transparent). Each one is a real little scale depositional sequence in relation to allocyclical processes by high frecuency eustatic variations during the last 6.000 yearses_ES
dc.publisherSociedad Geológica de Españaes_ES
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.subject.otherHigh resolution seismic profilees_ES
dc.subject.otherDeltaic sedimentationes_ES
dc.subject.otherContinental shelfes_ES
dc.subject.otherAlboran seaes_ES
dc.titleEstructuración sedimentaria de los cuerpos deltaicos holocenos del margen septentrional del mar de Alboránes_ES
dc.titleSedimentary structuration ofHolocene deltaic bodies in northem Alboran Sea margineng

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Atribución-NoComercial-SinDerivadas 3.0 España
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