Onderzoeksoutput

Welkom op het expertplatform!

Dit platform verschaft informatie en kennis omtrent de WL expertisedomeinen 'hydraulica en sediment', 'havens en waterwegen', 'waterbouwkundige constructies', 'waterbeheer' en 'kustbescherming' - gaande van WL medewerkers met hun expertise, het curriculum van deze instelling, tot publicaties, projecten, data (op termijn) en evenementen waarin het WL betrokken is.

Het WL onderschrijft het belang van "open access" voor de ontsluiting van haar onderzoeksresultaten. Lees er meer over in ons openaccessbeleid.

log in

• 
  People
• 
  Curriculum
• 
  Projects
• 
  Data sets
• 
  Publications
• 
  Events

[ meld een fout in dit record ]

mandje (1): toevoegen | toon

---

one publication added to basket [240770]

First evidence of a main channel generated by the Mediterranean Outflow Water after its exit from the Gibraltar Strait Hernández-Molina, F.J.; Llave, E.; Fontan, A.; Brackenridge, R.E.; Stow, D.A.V.; Ercilla, G.; Medialdea, T.; García, M.; Sandoval, N.; Preu, B.; Arlucea, M.P.; Nombela, M.A.; Alejo, I.; Francés, G.; Mena, A.; Casas, D.; Somoza, L.; León, R.; Vázquez, J.T.; Juan, C.; Van Rooij, D.; Matias, H.; Bruno, M.; Serra, N.; CONTOURIBER Team (2012). First evidence of a main channel generated by the Mediterranean Outflow Water after its exit from the Gibraltar Strait. Geo-Temas 13: 1813-1816 In: Geo-Temas. Sociedad Geológica de España: Madrid. ISSN 1576-5172

---

Beschikbaar in	Auteurs
VLIZ: Non-open access 262694 [ aanvragen ]

---

Trefwoord

Marien/Kust

---

Auteurs		Top
Hernández-Molina, F.J. Llave, E. Fontan, A. Brackenridge, R.E. Stow, D.A.V. Ercilla, G. Medialdea, T. García, M. Sandoval, N.	Preu, B. Arlucea, M.P. Nombela, M.A. Alejo, I. Francés, G. Mena, A. Casas, D. Somoza, L.	León, R. Vázquez, J.T. Juan, C. Van Rooij, D. Matias, H. Bruno, M. Serra, N. CONTOURIBER Team

---

Abstract

An extensive terrace comprising sandy sheeted drifts characterises the proximal sector (close to the Straits of Gibraltar) of the Contourite Depositional System (CDS) of the Gulf of Cadiz and the western continental margin of Portugal. A novel morphosedimentary study over this terrace has been executed based on new multibeam echosounder data, seismic profiles, and surficial sediments samples collected during the CONTOURIBER-1 Cruise (2010). Based on that study, an impressive large channel laterally connected with the central part of the Strait of Gibraltar (Camarinal Sill) has been identified. It is associated southwestward with a huge contourite levee (sand bank), which has been generated by overflow processes related to the Mediterranean Outflow Water (MOW). In the middle to the distal part of the terrace, there are other minor channels, erosional scour alignments and depositional features. The mapping of all these features coupled with CTD data allows to further understand the pathway and deceleration of the MOW, in addition to aid the conceptual identification of contourite terrace.

---

Alle informatie in het Integrated Marine Information System (IMIS) valt onder het VLIZ Privacy beleid

Top | Auteurs

IMIS is ontwikkeld en wordt gehost door het VLIZ.