NORWAY · WELLBORES · NPDID 1869

7122/4-1

Exploration · Wildcat · P&A · Shows · Esso Exploration and Production Norway A/S · PL 178

6 documents: reports, logs, and plots →

7122/4-1 is a wildcat exploration wellbore in the Barents Sea, drilled by Esso Exploration and Production Norway A/S, entered Nov 13, 1991, to 3,015 m in the Snadd Fm.

On the map →

3,015
m total depth
344.5
m water depth
Nov 13, 1991
entered · completed Jan 13, 1992
Snadd Fm
at total depth · Late Triassic
88.6
m of core in 4 cores
104
°C bottom-hole temperature

SODIR FACTPAGES · RECORD UPDATED MAR 1, 2026 · RELEASED JAN 13, 1994

On file for this wellbore

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

Drilling

Drilling facility
ARCADE FRONTIER · Semisub steel
Drilling days
62
Kelly bushing elevation
23.5 m
Maximum inclination
0°
Drilling permit
706-L
Licensing round
13
Plugged and abandoned
—
Core samples available
Yes
Cuttings samples available
Yes
Position · ED50
71.74735° N, 22.08511° E

Well history

WRITTEN BY THE NORWEGIAN OFFSHORE DIRECTORATE

General

Wildcat well 7122/4-1 was drilled in the Northern part of the Hammerfest Basin. The objective of the well was to test the Åsgard prospect, a large, tilted horst with Middle-Lower Jurassic sandstones of the Stø formation as the primary objective. The underlying Nordmela and Tubåen formations were also considered to have potential for reservoired hydrocarbons. The trap was formed by a horst structure dipping towards the North-Northwest. Well 7122/4-1 was the first well on this prospect.

Operations and results

Well 7122/4-1 was spudded with the semi submersible installation Sonate Arcade Frontier on 13 November 1991 and drilled to a total depth of 3015 m in the Triassic Snadd Formation. The well was drilled with seawater and gel down to 815 m, with KCl/polymer from 815 m to 2015 m, and with KCl/NaCl/Polymer from 2015 m to TD.

Good reservoir quality sandstones were encountered in the Stø and Nordmela Formations. Core analysis indicated generally good porosity and permeability. FMT's run in the Stø confirmed good permeability. However, analysis of the wire line logs indicated clearly that the Stø and Nordmela sandstones are water wet. The Tubåen Formation consisted primarily of sandstone, but was very thin in this well. Log analysis indicated that these sandstones are also water wet. Thin, tight sandstones (interbedded with claystone and siltstone) were present through much of the Triassic, generally decreasing in thickness with depth. From 2970 to 2990 m a Carnian sandstone was penetrated. The drill gas was higher through this zone than in any other sandstone in the well, averaging about 0.8 %. The cutting samples showed the reservoir quality to be quite poor, with no visible porosity. Numerous unsuccessful attempts with the FMT tool to obtain a pressure measurement indicated that this zone has extremely low permeability. This was confirmed by the log analysis.

Hydrocarbon shows were first observed in the Early Cret

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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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