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Pliocene and Quaternary seismic stacking pattern and distribution of contourites in the Algarve margin (Northern Gulf of Cadiz, Spain)

AuthorsLlave, Estefanía; Hernández-Molina, Francisco J.; Ercilla, Gemma ; Stow, D. A. V.; Medialdea, Teresa; Matias, Hugo
Issue Date2010
PublisherSociedad Geológica de España
CitationGeo-Temas 11: 103-104 (2010)
AbstractThree main changes in the sedimentary growth pattern within Pliocene and Quaternary contourite drifts in the Algarve margin are interpreted based on multichannel seismic profiles. Spatial distribution of major depocenters is mainly controlled by Pliocene tectonic structures, whose evolution controlled MOW behaviour. Nevertheless, after the Mid Pleistocene (MPR), the small-scale sedimentary stacking of the contourite drifts was more influenced by both climatic and sea-Ievel changes
DescriptionDeep-water Circulation: Processes & Products. International Congress 16-18 june 2010, Baiona, Pontevedra, Spain.-- 2 pages, 2 figures
Identifiersissn: 1576-5172
Appears in Collections:(ICM) Artículos
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