Relationship between the offlap-break location of Holocene prograding wedges on wave climate in southeastern Iberian Peninsula

View/Open
untranslated2010_Fernandez-Salasetal_CIESM (1).pdf (602.7Kb)
Identifiers
URI: http://hdl.handle.net/10508/6005
Export
Export to Ris.Exportar a BibTeX.
Share
Statistics
View Usage Statistics
Metadata
Show full item record
Authors
Fernández-Salas, L.M. (Luis Miguel); Lobo, F.J. (Francisco J.); Hernández-Molina, F.J. (Francisco Javier); Bárcenas-Gascón, P. (Patricia); Díaz-del-Río-Español, V. (Víctor)
Date
2010
Type
conference output
Keywords
Alboran Sea
Continental Shelf
Waves
Sediment Transport
Abstract
Wave 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.
Atribución-NoComercial-SinDerivadas 3.0 España
Except where otherwise noted, this item's license is described as Atribución-NoComercial-SinDerivadas 3.0 España