Show simple item record

dc.contributor.authorFernández-Salas, L.M. (Luis Miguel) es_ES
dc.contributor.authorLobo, F.J. (Francisco J.)es_ES
dc.contributor.authorHernández-Molina, F.J. (Francisco Javier)es_ES
dc.contributor.authorBárcenas-Gascón, P. (Patricia) es_ES
dc.contributor.authorDíaz-del-Río-Español, V. (Víctor) es_ES
dc.date.accessioned2014-11-21T09:22:48Z
dc.date.available2014-11-21T09:22:48Z
dc.date.issued2010es_ES
dc.identifier.urihttp://hdl.handle.net/10508/6005
dc.description.abstractWave climate exerts a significant influence on the development of Holocene sedimentary prograding wedges. This is demonstrated by the fact that near-bed orbital velocities between 0.10 and 0.14 m/s (threshold for resuspension) occur in the vicinity of the infralittoral prograding wedges (IPW) offlap-breaks during storm-weather conditions, but during medium wave energy conditions in the case of prodeltaic wedges.
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 Españaes_ES
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/es_ES
dc.subjectAlboran Sea
dc.subjectContinental Shelf
dc.subjectWaves
dc.subjectSediment Transport
dc.titleRelationship between the offlap-break location of Holocene prograding wedges on wave climate in southeastern Iberian Peninsulaes_ES
dc.typeconference outputes_ES
dc.identifier.bibliographicCitationCIESM. (10/05/2010 - 14/05/2010. Venecia (Italia)). 2010.es_ES
dc.publisher.centreCentro Oceanográfico de Cádizes_ES
dc.rights.accessRightsopen accesses_ES
dc.coverage.spatialStudyMediterranean Seaen_US
dc.coverage.spatialStudyWestern Mediterranean Seaen_US
dc.coverage.spatialStudyAlboran Seaen_US


Files in this item

untranslated

    Show simple item record

    Atribución-NoComercial-SinDerivadas 3.0 España
    Except where otherwise noted, this item's license is described as Atribución-NoComercial-SinDerivadas 3.0 España