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Horseshoe—Why
we drilled our third target first
CGX drilled its third-ranked and stratigraphic target, Horseshoe West,
June-July 2000 after the rig we'd contracted was forced off location
at Eagle, our primary turbidite target. The rig was mobilized from
Italy and arrived on the Eagle #1 location June 1.
At
12:15 am, June 3, Suriname Navy gunboats arrived at the Eagle location
with no running lights and ordered the Rig and the Tidewater supply
vessels to leave within 12 hours or face the consequences. For the
safety of the crews and vessels, CGX immediately ordered a move
to the Horseshoe West location, which was outside the zone Suriname
was disputing. The rig was placed on standby. Several days of discussion
between Guyana and Suriname produced no resolution of the conflict,
so CGX began drilling at Horseshoe West.
The maritime border dispute between Guyana and Suriname was resolved under the United Nations Laws of the Sea. On September 20, 2007, the International Tribunal on the Law of the Sea (ITLOS) issued its ruling in favour of Guyana. For more details on the resolution, please visit Maritime Border Resolution.
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Horseshoe Geology
The Horseshoe West target was a series of high-amplitude seismic
events with modest AVO anomalies mapped over a large area of 30,000
to 60,000 acres. The nearest well controls were the Arapaima #1
well about 70 miles (118 km) NNW and the I23-1/X well about 55
miles (92 km) east, where the lower-most Maastichtian was a series
of shales overlain by sandstones with minor carbonate and shales.
The geological hypothesis was the presence of up to 3 sand packages
on the flanks of the Berbice Canyon, which would be trapped by
the shales overlying the upper Cretaceous unconformity surface
seen in the Arapaima # 1 well.
We
encountered essentially 100% extremely clean and porous sand from
5,705 ft (1,739 m) to 10,748 ft (3,276 m) covering a gross interval
of 5,043 ft (1,537 m). The sand we encountered lies on the upper Cretaceous
unconformity surface. The age of the sand package is bracketed from
the lower Tertiary to the upper Cretaceous by the overlying and
underlying beds. The overlying shales, observed at the Arapaima
#1 and I23-1/X wells, didn't exist at Horseshoe West. The absence
of a shale seal is the principal reason for the lack of success
at this well and essentially eliminates any significant trap potential
associated with the unconformity and the Berbice Canyon. These factors
significantly downgrade our Horseshoe West, Horseshoe East and near-shore
stratigraphic targets.
The
massive sand thickness on the edge of the paleo-Berbice Canyon significantly
upgrades our Eagle and Wishbone turbidite targets downdip. |