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dc.contributor.authorLo Iacono, Claudioes_ES
dc.contributor.authorGuillén, Jorgees_ES
dc.date.accessioned2020-02-21T08:03:56Z-
dc.date.available2020-02-21T08:03:56Z-
dc.date.issued2004-
dc.identifier.citationRapports et procès-verbaux des réunions - Commission internationale pour l'exploration scientifique de la mer Méditerranée 37: 46 (2004)es_ES
dc.identifier.issn0373-434x-
dc.identifier.urihttp://hdl.handle.net/10261/201453-
dc.description1 page, 1 figurees_ES
dc.description.abstractSide scan sonar data were recorded across Marettimo island inner shelf (Egadi Islands; southern-western Tyrrhenian sea). The distribution and morphological characteristics of bedforms were analyzed across this sandy gravel inner shelf to examine possible forcing mechanisms. It is discussed that these morphological features could be produced by waves of period higher than 8 s and/or medium-high velocity bottom currentses_ES
dc.language.isoenges_ES
dc.publisherInternational Commission for the Scientific Exploration of the Mediterranean Seaes_ES
dc.rightsclosedAccesses_ES
dc.subjectGravel and sandy bedformses_ES
dc.subjectInner shelfes_ES
dc.subjectWaves and currentses_ES
dc.titleBedforms across a sandy-gravel continental inner shelf, Marettimo Island (Egadi Islands; Southern-Western Tyrrhenian Sea)es_ES
dc.typeinforme técnicoes_ES
dc.description.peerreviewedPeer reviewedes_ES
dc.relation.publisherversionhttp://ciesm.org/online/archives/abstracts/pdf/37/CIESM_Congress_2004_Barcelona_article_0046.htmes_ES
dc.relation.csices_ES
oprm.item.hasRevisionno ko 0 false*
dc.type.coarhttp://purl.org/coar/resource_type/c_18ghes_ES
item.cerifentitytypePublications-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.grantfulltextnone-
item.openairetypeinforme técnico-
item.fulltextNo Fulltext-
item.languageiso639-1en-
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