A mixed turbidite – contourite system related to a major submarine canyon: The Marquês de Pombal Drift (south‐west Iberian margin)

Author:

Mencaroni Davide12ORCID,Urgeles Roger1,Camerlenghi Angelo3,Llopart Jaume1,Ford Jonathan34,Sanchez Serra Cristina12,Meservy William12,GrÀcia EulÀlia1,Rebesco Michele3,Zitellini Nevio5

Affiliation:

1. Institut de Ciències del Mar (CSIC) Passeig Marítim de la Barceloneta, 37 Barcelona 08003 Spain

2. Universitat de Barcelona Barcelona 08028 Spain

3. National Institute of Oceanography and Applied Geophysics ‐ OGS Sgonico Trieste 34010 Italy

4. Università degli Studi di Trieste Trieste 34127 Italy

5. CNR‐National Research Council of Italy ISMAR‐Marine Science Institute Bologna 40129 Italy

Funder

H2020 Marie Skłodowska-Curie Actions

Publisher

Wiley

Subject

Stratigraphy,Geology

Reference141 articles.

1. Contourite vs gravity-flow deposits of the Pleistocene Faro Drift (Gulf of Cadiz): Sedimentological and mineralogical approaches

2. Observations of the Mediterranean outflow—I mixing in the Mediterranean outflow

3. A physical and chemical description of the Mediterranean outflow in the Gulf of Cadiz

4. Amo A. Reffray G. Sotillo M.G. Aznar R.andGuihou K.(2020)Atlantic ‐Iberian Biscay Irish‐ Ocean Physics Analysis and Forecast Product: IBI_ANALYSIS_FORECAST_PHYS_005_001. Prod. User Man. (7.0) 1–45.https://resources.marine.copernicus.eu/documents/PUM/CMEMS‐IBI‐PUM‐005‐001.pdf.

5. Newly recognized turbidity current structure can explain prolonged flushing of submarine canyons

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