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General
Block 2/6 is structurally located on the eastern margin of the Norwegian part of the Feda Graben. The block partly covers the Piggvar Terrace, the metamorphic Mandal high and the northwestern part of the Søgne basin.
Well 2/6-5 is located in the central western part of the block, high on a structural closure defined on Top Shetland Group
The main objective of well 2/6-5 was to test the presence of hydrocarbons and reservoir properties within the primary target intervals of the Shetland Group, located within a structural closure above the northern part of the Mandal High. It was prognosed approximately 40 m below the distinct Late Cretaceous Top Ekofisk Formation reflector.
Reservoir units were expected in several intervals, some in pressure communication and some not. A possible secondary target of sediment fill in the interval between the Shetland Group and the basement topography would be penetrated before reaching TD in metamorphic rocks. However, this possible wedge was defined on a poor seismic response and could represent intra basement reflectivity. The well was planned as a possible future producer.
Operations and results
Exploration well 2/6-5 was spudded by the semi-submersible installation "Deepsea Bergen" 17 November 1996 and drilled to TD at 3260 m in metamorphic rocks. The well was drilled with a sea water/bentonite mud system down through the 12 1/2" hole section to 2515 m. The deeper part of the well was drilled with a KCL polymer glycol mud system.
Above the Shetland
Group the formation tops and lithologies were drilled within the uncertainty
limits of the prognosis. The Tertiary succession (including Quaternary) was
found to be 2872 m thick. The Nordland Group was 1404.7 m thick and consisted
of clay/claystones and sands. Top of the Hordaland Group was encountered at
1499.5 m and the Group was found to be 1229.4 m thick, generally consisting of
reactive clay
wlbHistoryDateUpdated: 2016-07-06T00:00:00