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General
Wildcat well 1/6-1 is located ca 15 km northwest of the Ekofisk Field in the southern Norwegian North Sea. It was drilled in a crestal position on a large chalk structure shared between Norske Shell's block l/6 and Phillips' block 2/4, the Ekofisk block. Phillips participated in drilling this well on a 50/50 basis. The primary objective was to investigate Danian and Maastrichtian chalk prospects. Secondary objective was to evaluate possible sand developments in the Paleocene and the Lower Cretaceous or older units. Planned total depth was 4572 m (1500 ft).
Operations and results
Well 1/6-1 was spudded with the jack-up installation Zapata Nordic on 10 July 1972 and drilled to TD at 4822 m in the Late Permian Zechstein Group. No major technical problems were encountered in the operations and the drilling of this deep well was within the prognosed time schedule. The drill string stuck at 228 m. After working the string and spotting pipe-free/diesel the string came loose. Some highly porous limestone intervals (1 - 8 m thick) resulted in lost circulation problems. The pipe stuck at 3456 m, but was freed after spotting with pipe-free/diesel. The well was drilled with seawater down to 448 m, with seawater/lignosulphonate and a shale inhibitor (shalock) from 448 m to 1586 m, and with seawater/lignosulphonate/ligcon (caustisized lignite) from 1586 m to TD.
Reservoir development was encountered
only in the Chalk Formations, with hydrocarbon-bearing intervals being
developed in both the Danian and Late Cretaceous. Four hydrocarbon-bearing
intervals were encountered and tested within the Chalk, but only one zone in
the Maastrichtian (Tor Formation), yielded commercial flows of gas and
condensate. Reservoir developments in the Danian (Ekofisk Formation) and
earlier Maastrichtian (Hod Formation) were found to be considerably less
favourable in l/6-l than in the adjacent Ekofisk and West Ekofisk field. The
Early Cretaceous (Valanginian) w
wlbHistoryDateUpdated: 2016-07-06T00:00:00