IMIS

Publicaties | Instituten | Personen | Datasets | Projecten | Kaarten
[ meld een fout in dit record ]mandje (0): toevoegen | toon Print deze pagina

Sediment drifts and deep-sea channel systems, Antarctic Peninsula Pacific Margin
Rebesco, M.; Pudsey, C.J.; Canals, M.; Camerlenghi, A.; Barker, R.R.; Estrada, R.; Giorgetti, A. (2002). Sediment drifts and deep-sea channel systems, Antarctic Peninsula Pacific Margin, in: Stow, D.A.V. et al. Deep-water contourite systems: Modern drifts and ancient series, seismic and sedimentary characteristics. Geological Society Memoir, 22: pp. 353-371. https://dx.doi.org/10.1144/GSL.MEM.2002.022.01.25
In: Stow, D.A.V. et al. (Ed.) (2002). Deep-water contourite systems: Modern drifts and ancient series, seismic and sedimentary characteristics. Geological Society Memoir, 22. The Geological Society: London. ISBN 1-86239-092-4. vi, 464 pp., meer
In: Geological Society Memoir. Geological Society: London. ISSN 0435-4052; e-ISSN 2041-4722, meer

Beschikbaar in  Auteurs | Datasets 

Trefwoord
    Marien/Kust

Auteurs  Top | Datasets 
  • Rebesco, M.
  • Pudsey, C.J.
  • Canals, M.
  • Camerlenghi, A.
  • Barker, R.R.
  • Estrada, R.
  • Giorgetti, A.

Abstract
    Twelve sedimentary mounds are identified on the upper continental rise of the Pacific Margin of the Antarctic Peninsula. All these mounds are produced by a varying degree of interaction of along-slope bottom water flow with down-slope turbidity currents. These mounds provide a complete range of intermediates between two end members: the sediment drift and the channel levee. Surface sediments on drift 7 suggest that the mechanisms for the supply and transport of sediment include entrainment of material from turbidity currents within ambient bottom currents, and pelagic settling from the sea surface, including biogenic and glacially derived material. The long-lasting activity of these mechanisms is documented by the data provided by four DSDP and ODP drill sites. Bathymetric and seismic data, both at a large, comprehensive scale and at a small, detailed scale, show the geometry of the sedimentary mounds and their relationships with the adjacent turbidity current channel systems. These data allow the determination of some diagnostic criteria to identify the sediment drifts.

Datasets (2)
  • Global contourite distribution database, version 2, meer
  • Global contourite distribution database, version 3, meer

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