IMIS

Publicaties | Instituten | Personen | Datasets | Projecten | Kaarten
[ meld een fout in dit record ]mandje (1): toevoegen | toon Print deze pagina

one publication added to basket [302081]
Contourite drift types and their distribution in the North and South Atlantic Ocean basins
Faugeres, J.-C.; Mézerais, M.L.; Stow, D.A.V. (1993). Contourite drift types and their distribution in the North and South Atlantic Ocean basins. Sediment. Geol. 82(1-4): 189-203. https://dx.doi.org/10.1016/0037-0738(93)90121-k
In: Sedimentary Geology. Elsevier: Tokyo; Oxford; New York; London; Amsterdam. ISSN 0037-0738; e-ISSN 1879-0968, meer
Peer reviewed article  

Beschikbaar in  Auteurs | Datasets 

Auteurs  Top | Datasets 
  • Faugeres, J.-C.
  • Mézerais, M.L.
  • Stow, D.A.V.

Abstract
    Patterns of sediment accumulation under the control of deep bottom currents depend on interacting factors: intensity of the regional deep circulation, morphology of the sea-floor, Coriolis effects, abundance of terrigenous and biogenic supplies, subsequent turbidity of deep nepheloid layers, and depth of the CCD. Based on many examples of bottom current deposits, from the Atlantic and from other oceans, we recognise three major types of contourite accumulation: (1) giant elongate drifts, (2) contourite sheets, and (3) channel-related drifts. They generally occur in distinct topographic settings and show different geometries, facies and rates of deposition. In the North Atlantic, strong bottom circulation, an open basin system and high sediment supply have led to the construction of large elongate contourite drifts, which have striking relief (200–1000 m) above the surrounding sea-floor and are composed of muddy contourites, rich in calcareous pelagic material. In the South Atlantic, strong bottom-currents are often trapped in gyre-like circulation patterns around topographically closed basins or are accelerated through deep, narrow, connecting passages. The resulting deposits are mainly extensive contourite sheets, covered by fields of large sediment waves, and channel-related drifts, including “contourite fans” constructed at the downstream exit of deep passages.

Datasets (2)
  • Flanders Marine Institute; Renard Centre of Marine Geology - Ugent (2018). Global contourite distribution database, version 2. Available online at https://www.marineregions.org, meer
  • Flanders Marine Institute; Renard Centre of Marine Geology - Ugent (2019). Global contourite distribution database, version 3. Available online at https://www.marineregions.org, meer

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