Stratigraphic and Reservoir Architecture of Tectonically-Confined Turbidite Ramps – The Example of the Grès d'Annot System (Eocene - Oligocene, French Alps)

P. Joseph; E. Du Fornel; T. Euzen; F. Guillocheau; C. Robin

doi:10.3997/2214-4609-pdb.3.A032

Stratigraphic and Reservoir Architecture of Tectonically-Confined Turbidite Ramps – The Example of the Grès d'Annot System (Eocene - Oligocene, French Alps)
By P. Joseph, E. Du Fornel, T. Euzen, F. Guillocheau and C. Robin
Publisher: European Association of Geoscientists & Engineers
Source: Conference Proceedings, 66th EAGE Conference & Exhibition, Jun 2004, cp-3-00222
DOI: https://doi.org/10.3997/2214-4609-pdb.3.A032

Abstract

A032 Stratigraphic and reservoir architecture of tectonically-confined turbidite ramps : the example of the Grès d’Annot system (Eocene - Oligocene French Alps) 1 P. JOSEPH 1 E. DU FORNEL 1-2 T. EUZEN 1 F. GUILLOCHEAU 2 and C. ROBIN 2 ¹ Institut Français du Pétrole 1 et 4 avenue de Bois Préau 92852 Rueil Malmaison cedex France. ² Géosciences Rennes Université de Rennes 1 Campus de Beaulieu 35042 Rennes France. Summary For a long time the Grès d’Annot system of South East France has been considered as a classic example of a canyon-fed submarine fan settled during a period of

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2004-06-07

2024-09-10

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Stratigraphic and Reservoir Architecture of Tectonically-Confined Turbidite Ramps – The Example of the Grès d'Annot System (Eocene - Oligocene, French Alps)

Abstract

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The natural combination of full and image‐based waveform inversion

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