Please use this identifier to cite or link to this item: http://hdl.handle.net/10553/44121
DC FieldValueLanguage
dc.contributor.authorAlbarracín, Silviaen_US
dc.contributor.authorAlcántara-Carrió, Javieren_US
dc.contributor.authorMontoya-Montes, Isabelen_US
dc.contributor.authorFontán-Bouzas, Ángelaen_US
dc.contributor.authorSomoza, Luisen_US
dc.contributor.authorAmos, Carl L.en_US
dc.contributor.authorRey Salgado, Jorgeen_US
dc.contributor.otherMontoya-Montes, Isabel-
dc.contributor.otherFontan Bouzas, Angela-
dc.contributor.otherSomoza, Luis-
dc.contributor.otherAlcantara-Carrio, Javier-
dc.contributor.otherFontan Bouzas, Angela-
dc.date.accessioned2018-11-21T20:23:22Z-
dc.date.available2018-11-21T20:23:22Z-
dc.date.issued2014en_US
dc.identifier.issn1385-1101en_US
dc.identifier.urihttp://hdl.handle.net/10553/44121-
dc.description.abstractThe presence of fossil or relict bedforms is common in the Quaternary fill of modern continental shelf due to sea level oscillations, tectonic subsidence and migration of associated sedimentary facies. The continental margin of the Gulf of Valencia has been strongly influenced by glacio-eustasy and neotectonics. High-resolution multibeam bathymetry data, seismic reflection profiles and box core samples were collected across the continental shelf of the Gulf of Valencia during the DERIVA cruises carried out in 2010 and 2011. The integrated analysis of this data set and high-resolution mapping of the relict bedforms on the Valencian continental shelf, ranging between 50 and 90 m allowed the study of previously identified system of sand waves located in front of the present-day Albufera de Valencia lagoon. The system is composed of 27 ridges with a NNE–SSW orientation, i.e. oblique to the present shoreline, in which the lateral horns point backwards. These sand waves can reach 10 m in height and 3 km in length resulting in a maximum slope of 6°. According to seismic stratigraphic and relative sea level curve reconstructions, these sand waves were formed during the Younger Dryas (~ 12–10 ky BP). Consequently, they have been classified as Holocene sand waves associated with coastal sedimentary evolution.en_US
dc.languageengen_US
dc.relation.ispartofJournal of Sea Researchen_US
dc.sourceJournal Of Sea Research [ISSN 1385-1101], v. 93, p. 33-46en_US
dc.subject2510 Oceanografíaen_US
dc.subject251007 Oceanografía físicaen_US
dc.subject.otherHoloceneen_US
dc.subject.otherSeismic stratigraphyen_US
dc.subject.otherContinental shelfen_US
dc.subject.otherSand wavesen_US
dc.subject.otherSubaqueous dunesen_US
dc.subject.otherWestern mediterraneanen_US
dc.titleRelict sand waves in the continental shelf of the Gulf of Valencia (Western Mediterranean)en_US
dc.typeinfo:eu-repo/semantics/articleen_US
dc.typeArticleen_US
dc.identifier.doi10.1016/j.seares.2013.12.014en_US
dc.identifier.scopus2-s2.0-84906315294-
dc.identifier.isi000342244700006-
dcterms.isPartOfJournal Of Sea Research-
dcterms.sourceJournal Of Sea Research[ISSN 1385-1101],v. 93, p. 33-46-
dc.contributor.authorscopusid55503811900-
dc.contributor.authorscopusid6507201462-
dc.contributor.authorscopusid25626392800-
dc.contributor.authorscopusid55505042200-
dc.contributor.authorscopusid56256960600-
dc.contributor.authorscopusid7103050546-
dc.contributor.authorscopusid56015966800-
dc.description.lastpage46en_US
dc.description.firstpage33en_US
dc.relation.volume93en_US
dc.investigacionCienciasen_US
dc.type2Artículoen_US
dc.identifier.wosWOS:000342244700006-
dc.contributor.daisngid6879404-
dc.contributor.daisngid1808171-
dc.contributor.daisngid2870850-
dc.contributor.daisngid5123747-
dc.contributor.daisngid350799-
dc.contributor.daisngid323385-
dc.contributor.daisngid4095861-
dc.identifier.investigatorRIDD-9245-2013-
dc.identifier.investigatorRIDC-3556-2015-
dc.identifier.investigatorRIDC-1400-2010-
dc.identifier.investigatorRIDD-9417-2013-
dc.identifier.investigatorRIDNo ID-
dc.utils.revisionen_US
dc.identifier.ulpgcen_US
dc.description.sjr0,977
dc.description.jcr1,99
dc.description.sjrqQ1
dc.description.jcrqQ2
dc.description.scieSCIE
item.fulltextSin texto completo-
item.grantfulltextnone-
crisitem.author.deptGIR IOCAG:Geología Aplicada y Regional-
crisitem.author.deptIU de Oceanografía y Cambio Global-
crisitem.author.deptDepartamento de Física-
crisitem.author.orcid0000-0001-5401-3841-
crisitem.author.parentorgIU de Oceanografía y Cambio Global-
crisitem.author.fullNameMontoya Montes, Isabel-
Appears in Collections:Artículos
Show simple item record

Google ScholarTM

Check

Altmetric


Share



Export metadata



Items in accedaCRIS are protected by copyright, with all rights reserved, unless otherwise indicated.