Vertical grain-size variability within a turbidite levee: Autocyclicity or allocyclicity? A case study from the Rhône neofan, Gulf of Lions, Western Mediterranean

Author:

Dennielou Bernard,Huchon Agnès,Beaudouin Célia,Berné Serge

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology,Oceanography

Reference59 articles.

1. The Late-Quaternary climatic signal recorded in a deep-sea turbiditic levee (Rhône Neofan, Gulf of Lions, NW Mediterranean): palynological constraints;Beaudouin;Sediment. Geol.,2004

2. Present-day rhythmic deposition in the Grand Rhône prodelta (NW Mediterranean) according to high-resolution pollen analyses;Beaudouin;J. Coast. Res.,2005

3. Carte morpho-bathymétrique du Golfe du Lion. Ifremer-Région Languedoc-Roussillon, Brest;Berné,2001

4. Architecture and depositional pattern of the Rhône Neofan and recent gravity activity in the Gulf of Lions (Western Mediterranean);Bonnel;Mar. Pet. Geol.,2005

5. Sedimentology of Some Flysh Deposits: A Graphic Approach to Facies Interpretation;Bouma,1962

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