NORWAY · WELLBORES · NPDID 8

7120/12-3

Exploration · Wildcat · P&A · Gas · Norsk Hydro Produksjon AS · PL 061

6 documents: reports, logs, and plots →

7120/12-3 is a wildcat exploration wellbore in the Barents Sea, drilled by Norsk Hydro Produksjon AS, entered Mar 16, 1983, to 2,523 m in the Fruholmen Fm.

Discovery 7120/12-3 (Alke Nord) · On the map →

2,523
m total depth · 2,522 m vertical
185
m water depth
Mar 16, 1983
entered · completed May 5, 1983
Fruholmen Fm
at total depth · Late Triassic
18
m of core in 1 core
118
°C bottom-hole temperature

SODIR FACTPAGES · RECORD UPDATED MAR 1, 2026 · RELEASED MAY 5, 1985

On file for this wellbore

What the Directorate holds from this wellbore. Each opens the section that lists it.

Drilling

Drilling facility
TREASURE SCOUT · Semisub steel
Drilling days
51
Kelly bushing elevation
23 m
Maximum inclination
3.0999999°
Drilling permit
367-L
Licensing round
5
Plugged and abandoned
—
Core samples available
Yes
Cuttings samples available
Yes
Position · ED50
71.19536° N, 20.77881° E
Hydrocarbons in
Stø Fm · Middle Jurassic

Well history

WRITTEN BY THE NORWEGIAN OFFSHORE DIRECTORATE

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

Around this wellbore

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About this data

Norwegian Offshore Directorate (Sodir) FactPages, mirrored nightly and used under the Norwegian Licence for Open Government Data (NLOD). Depths are metres along the wellbore from the kelly bushing unless a row gives its own unit; older cores are filed in feet. A zero the Directorate files for an unmeasured pressure, density, or temperature is shown as a dash.

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