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Dynamics of shoreface-connected and inactive sand ridges on a shelf, Part 2: The role of sea level rise and associated changes in shelf geometry

Autor
Nnafie, A.; de Swart, H.; Calvete, D.; Garnier, R.
Tipus d'activitat
Article en revista
Revista
Continental shelf research
Data de publicació
2015-08-01
Volum
104
Pàgina inicial
63
Pàgina final
75
DOI
https://doi.org/10.1016/j.csr.2015.05.009 Obrir en finestra nova
Repositori
http://hdl.handle.net/2117/28309 Obrir en finestra nova
URL
http://www.sciencedirect.com/science/article/pii/S0278434315001405 Obrir en finestra nova
Resum
Many inner continental shelves are characterized by the presence of large rhythmic bedforms, such as shoreface-connected ridges and the more offshore located sand ridges, which have heights of several meters and are spaced several kilometers apart. This study focuses on explaining the observed orientation difference between shoreface-connected sand ridges and the more offshore located ridges. For this, an existing idealized morphodynamic model is used, but modified such that sea level rise simul...
Citació
Nnafie, A. [et al.]. Dynamics of shoreface-connected and inactive sand ridges on a shelf, Part 2: The role of sea level rise and associated changes in shelf geometry. "Continental shelf research", Agost 2015, vol. 104, p. 63-75.
Paraules clau
Holocene, Sand ridges, connected, inactive, inner shelf, sea level rise
Grup de recerca
DF - Dinàmica de Fluids: formació d'estructures i aplicacions geofísiques

Participants

  • Nnafie, Abdel  (autor)
  • de Swart, Huib E.  (autor)
  • Calvete Manrique, Daniel  (autor)
  • Garnier, Roland Charles  (autor)

Arxius