2003
DOI: 10.1144/1354-079302-514
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4D integrated technologies for deep-water turbidite reservoirs:from petrophysics to fluid flow simulation

Abstract: Petrobras has been developing its 4D seismic technological programme since 1998, focused on the Brazilian deep-water fields in the Campos Basin, and considering the technical, operational and economic challenges involved in the development plan and reservoir management in this environment. The first step was to align the objectives of the project with the company goals for the following 15 years, in terms of earnings growth, production growth and reserves replacement. This information guided how the … Show more

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Cited by 2 publications
(2 citation statements)
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“…2003) and the Pliocene sands of the South Timbalier Field, Gulf of Mexico (Burkhart, Hoover and Flemings 2000). 4D seismic potential for fields lying in deep water has also been demonstrated for turbidite developments in the Oligocene/Miocene of the Campos Basin, Brazil (Santos et al . 2003) and the Palaeocene of the Girassol Field in West Africa (Beydoun et al .…”
Section: Introductionmentioning
confidence: 90%
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“…2003) and the Pliocene sands of the South Timbalier Field, Gulf of Mexico (Burkhart, Hoover and Flemings 2000). 4D seismic potential for fields lying in deep water has also been demonstrated for turbidite developments in the Oligocene/Miocene of the Campos Basin, Brazil (Santos et al . 2003) and the Palaeocene of the Girassol Field in West Africa (Beydoun et al .…”
Section: Introductionmentioning
confidence: 90%
“…Examples are the Palaeocene sands of the West of Shetlands area of the North Sea (Parr, Marsh and Griffin 2000), the Nelson Field, central North Sea and the Pliocene sands of the South Timbalier Field, Gulf of Mexico (Burkhart, Hoover and Flemings 2000). 4D seismic potential for fields lying in deep water has also been demonstrated for turbidite developments in the Oligocene/Miocene of the Campos Basin, Brazil (Santos et al 2003) and the Palaeocene of the Girassol Field in West Africa (Beydoun et al 2002). Most of these fields are characterized in the 4D sense by a strong signature from clean, relatively unconsolidated sands with moderate-to-high porosity and an excellent contrast in acoustic properties between the displacing and displaced reservoir fluids.…”
Section: Introductionmentioning
confidence: 99%