All Days 2007
DOI: 10.4043/19085-ms
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Golfinho Field-Discovery, Development, and Future Prospects

Abstract: TX 75083-3836, U.S.A., fax 01-972-952-9435. Abstract

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Cited by 6 publications
(7 citation statements)
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“…Submarine channels and lobes identified in the ESB comprise reservoir-prone elements similar to proven exploration targets in SE Brazil. For instance, Canyon C0 is comparable to the Golfinho Field and Regência discoveries in the ESB (Bruhn and Walker, 1997;Fiduk et al, 2004;Vieira et al, 2007;Vincentelli et al, 2007). Discoveries in Eocene and Oligocene strata of These lobes show thickness values similar to producing deepwater reservoirs, in the order of 20 to 30 m (Hardage et al, 1998;Prather et al, 2000;Puckette and Al-Shaieb, 2003).…”
Section: Distribution Of Compartmentalised Sand-prone Strata In the Esbmentioning
confidence: 73%
“…Submarine channels and lobes identified in the ESB comprise reservoir-prone elements similar to proven exploration targets in SE Brazil. For instance, Canyon C0 is comparable to the Golfinho Field and Regência discoveries in the ESB (Bruhn and Walker, 1997;Fiduk et al, 2004;Vieira et al, 2007;Vincentelli et al, 2007). Discoveries in Eocene and Oligocene strata of These lobes show thickness values similar to producing deepwater reservoirs, in the order of 20 to 30 m (Hardage et al, 1998;Prather et al, 2000;Puckette and Al-Shaieb, 2003).…”
Section: Distribution Of Compartmentalised Sand-prone Strata In the Esbmentioning
confidence: 73%
“…4). A regional unconformity of Late Maastrichtian age marks the upper boundary of the unit (Vieira et al, 2007).…”
Section: Unit S5 (Late Santonian To Maastrichtian)mentioning
confidence: 99%
“…Unit S5 comprises low-moderate amplitude strata above Unit S4. The lower boundary of the unit is marked by an unconformity related to the incision of a Late Cretaceous channel system (horizon H4 -Golfinho Field; Vieira et al, 2007;Alves, 2012) (Fig. 5).…”
Section: Unit S5 (Late Santonian To Maastrichtian)mentioning
confidence: 99%
“…A major unconformity related to the incision of a Late Santonian to Maastrichtian channel system is observed above low-amplitude strata in K82-K88 (Golfinho Field, Vieira et al, 2007). strata into listric, salt-detached faults is observed below the unconformity ( Fig.…”
Section: K90-k130 Sequence (Late Santonian To Maastrichtian)mentioning
confidence: 97%