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General
Well 7120/12-3 is located in the Hammerfest Basin, south of the Snøhvit area. The primary objective was to test a sandstone reservoir of Middle to Early Jurassic age on a structure (Alke North) separate from the Alke Structure tested in well 7120/12-1 and 7120/12-2. A secondary objective was to test Middle Triassic sandstones, providing the Jurassic reservoir proved a gas column greater than 60 m. The well was planned to be drilled to 2498 + 30 m or to 3312 +100 m if the Jurassic test was positive.
Operations and results
Wildcat well 7120/12-3 was spudded with the semi-submersible installation on 16 March 1983 and drilled to TD at 2523 m in the Late Triassic Fruholmen Formation. Swelling shales and some tight hole problems occurred in the 17 1/2" section; otherwise no significant problems were encountered during drilling. The well was drilled using seawater / bentonite / hi-vis pills down to 605 m and with a gypsum / polymer mud from 605 m to TD.
The Middle to Early Jurassic sandstone
reservoir was found gas bearing from 2157.5 to 2182.5 m (upper part of Stø
Formation) where the gas/water contact was established. The reservoir consisted
of very fine to fine, relatively homogeneous and clean sandstones made up of
clear quartz with traces of mica, glauconite and carbonaceous material. From
wire line logs the net pay was calculated to be 24 m, with an average porosity
of 17 % and an average water saturation of 17 %. Traces of very weak shows were
described from cuttings and sidewall cores between 1945 m to 2148.5 m in
shales of the Late Jurassic Hekkingen and Fuglen Formation, reflecting the
high organic content of these shales. Direct shows were only seen in the lower
part of the gas-bearing reservoir from 2170 m to 2182.5 m. They appeared on
sandstones as traces of dull yellow fluorescence with weak slow streaming dull
yellow to white crush cut, no stain or residue were detected. Very weak shows
were detected in shale
wlbHistoryDateUpdated: 2016-05-19T00:00:00